|"SOI5 description"|||"THE WORTHEN SERIES CONSISTS OF WELL DRAINED SOILS FORMED IN LOCAL ALLUVIUM ON FOOTSLOPES, TERRACES AND ALLUVIAL FANS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND DARK BROWN SILT LOAM 29 INCHES THICK. THE SUBSOIL IS BROWN AND DARK YELLOWISH BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 12 PERCENT. CROPLAND IS THE MAIN USE."|"197578:290158"|"197578:186514"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Worthen component makes up 91 percent of the map unit. Slopes are 0 to 2 percent. This component is on alluvial fans. The parent material consists of silty valley side alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"197578:290158"|"197578:1241892"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Vesser soil is a minor component."|"197578:857955"|"197578:1241895"
|"SOI5 description"|||"THE VESSER SERIES CONSISTS OF SOMEWHAT POORLY OR POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM UNDER GRASSES ON HIGH BOTTOM LANDS, FOOTSLOPES AND FANS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 12 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAY AND DARK GRAY SILT LOAM 19 INCHES THICK. THE SUBSOIL IS DARK GRAY AND VERY DARK GRAY SILTY CLAY LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"197578:857955"|"197578:513223"
|"SOI5 description"|||"THE LITTLETON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON TERRACES, ALLUVIAL FANS AND UPLAND TOE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAY AND VERY DARK GRAYISH BROWN SILT LOAM 26 INCHES THICK. THE SUBSOIL IS BROWN MOTTLED SILT LOAM 17 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"197578:867055"|"197578:521349"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Littleton soil is a minor component."|"197578:867055"|"197578:1241894"
|"SOI5 description"|||"THE KENDALL SERIES, FLOODED, CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY MATERIAL AND STRATIFIED OUTWASH ON TERRACES. THE SURFACE LAYER IS BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE IS LIGHT BROWNISH GRAY SILT LOAM 5 INCHES THICK. THE SUBSOIL IS BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM IN UPPER 29 INCHES AND PALE BROWN MOTTLED SILT LOAM IN LOWER 9 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"197578:871593"|"197578:527011"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Kendall soil is a minor component."|"197578:871593"|"197578:1241893"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Oil waste land is a miscellaneous area."|"198880:289333"|"198880:1241833"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, November, December. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 4w.  This soil meets hydric criteria."|"198881:265214"|"198881:1241918"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198881:265214"|"198881:169239"
|"SOI5 description"|||"THE ARENZVILLE SERIES, MODERATELY WET, CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN SILT LOAM ALLUVIUM OVER DARK COLORED BURIED SOILS ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 10 INCHES THICK. THE SUBSTRATUM IS 15 INCHES OF BROWN, DARK GRAYISH BROWN AND VERY DARK GRAYISH BROWN SILT LOAM STRATIFIED WITH LENSES OF VERY FINE SAND OVER 15 INCHES OF A BLACK MOTTLED SILT LOAM BURIED SURFACE LAYER OVER DARK GRAYISH BROWN MOTTLED SILT LOAM WITH FEW LENSES OF SAND. SLOPES RANGE FROM 0 TO 5 PERCENT. PASTURELAND IS THE MAIN USE."|"198882:264386"|"198882:168500"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Arenzville component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during January, February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198882:264386"|"198882:1241919"
|"SOI5 description"|||"THE BIRDS SERIES DRAINED CONSISTS OF POORLY DRAINED SOILS FORMED UNDER FOREST VEGETATION IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE NEXT 16 INCHES IS GRAY MOTTLED SILT LOAM TRANSITIONAL LAYER. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198883:1568271"|"198883:1244144"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Birds component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198883:1568271"|"198883:1244145"
|"SOI5 description"|||"THE DUPO SERIES, DRAINED, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN RECENT, LIGHT-COLORED, SILTY ALLUVIUM OVERLYING DARK, CLAYEY SOILS ON FLOOD PLAINS. THE SURFACE SOIL IS BROWN SILT LOAM 9 INCHES THICK. THE SUBSTRATUM IS BROWN SILT LOAM IN UPPER 16 INCHES AND VERY DARK GRAY, DARK GRAY, AND GRAY SILTY CLAY AND CLAY IN LOWER 55 INCHES. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. CROPLAND IS THE MAIN USE."|"198883:264390"|"198883:168504"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Dupo component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium over clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198883:264390"|"198883:1241920"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198884:1568254"|"198884:1243970"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198884:1568254"|"198884:1243971"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"198884:1568263"|"198884:1243989"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198884:1568263"|"198884:1243990"
|"SOI5 description"|||"THE SHAFFTON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOAMY ALLUVIUM ON FLOOD PLAINS AND LOW STREAM TERRACES. THE SURFACE SOIL IS A BLACK AND VERY DARK GRAYISH BROWN LOAM 13 INCHES THICK. THE SUBSOIL IS BROWN, DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED LOAM IN UPPER 23 INCHES AND GRAYISH BROWN LOAMY SAND IN LOWER 3 INCHES. THE SUBSTRATUM IS 6 INCHES OF GRAY SILTY CLAY LOAM OVER GRAYISH BROWN COARSE SAND. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND PASTURELAND."|"198884:264391"|"198884:168505"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Shaffton component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198884:264391"|"198884:1241922"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198885:1568253"|"198885:1243969"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198885:1568253"|"198885:1243968"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198885:1568278"|"198885:1244340"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198885:1568278"|"198885:1244341"
|"SOI5 description"|||"THE TICE SERIES, COMMONLY FLOODED, CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 14 INCHES THICK. THE MOTTLED SILTY CLAY LOAM SUBSOIL IS DARK GRAYISH BROWN IN UPPER 5 INCHES, BROWN IN NEXT 16 INCHES AND DARK GRAYISH BROWN TO A DEPTH OF 80 INCHES. SLOPES RANGE FROM 0 TO 4 PERCENT. CROPLAND IS THE MAIN USE."|"198885:264392"|"198885:168506"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Tice component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198885:264392"|"198885:1241925"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ambraw component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198886:264393"|"198886:1241928"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198886:264393"|"198886:168507"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"198887:1568262"|"198887:1243987"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198887:1568262"|"198887:1243988"
|"SOI5 description"|||"THE LANDES SERIES, WELL DRAINED, CONSISTS OF WELL DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN FINE SANDY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK BROWN AND BROWN LOAM IN UPPER 9 INCHES, BROWN AND DARK YELLOWISH BROWN FINE SANDY LOAM IN NEXT 9 INCHES AND DARK YELLOWISH BROWN AND BROWN LOAMY SAND IN LOWER 4 INCHES. THE SUBSTRATUM IS YELLOWISH BROWN SAND WITH FEW FINE GRAVEL. SLOPES RANGE FROM 0 TO 7 PERCENT. CROPLAND IS THE MAIN USE."|"198887:264394"|"198887:168508"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Landes component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on flood plains. The parent material consists of sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198887:264394"|"198887:1241929"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198888:1568255"|"198888:1243972"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198888:1568255"|"198888:1243973"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Rocher component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on flood plains. The parent material consists of sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat excessively drained.  Water movement in the most restrictive layer is high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 18 percent."|"198888:264383"|"198888:1241915"
|"SOI5 description"|||"THE ROCHER SERIES CONSISTS OF SOMEWHAT EXCESSIVELY DRAINED SOILS FORMED IN CALCAREOUS STRATIFIED ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS DARK BROWN LOAM 5 INCHES THICK. THE SUBSTRATUM IS STRATIFIED BROWN VERY FINE SANDY LOAM, LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAMY VERY FINE SAND AND LIGHT YELLOWISH BROWN LOAMY FINE SAND. SLOPES RANGE FROM 0 TO 7 PERCENT. CROPLAND IS THE MAIN USE."|"198888:264383"|"198888:168497"
|"SOI5 description"|||"THE BIRDS SERIES DRAINED CONSISTS OF POORLY DRAINED SOILS FORMED UNDER FOREST VEGETATION IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE NEXT 16 INCHES IS GRAY MOTTLED SILT LOAM TRANSITIONAL LAYER. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198889:1568270"|"198889:1244142"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Birds component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198889:1568270"|"198889:1244143"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Wakeland component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198889:264395"|"198889:1241933"
|"SOI5 description"|||"THE WAKELAND SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS ON FLOOD PLAINS AND FLOODPLAIN STEPS. THEY FORMED IN SILTY ALLUVIUM. THE SURFACE LAYER IS GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM 53 INCHES THICK. DOMINANT USE IS CROPLAND."|"198889:264395"|"198889:168509"
|"SOI5 description"|||"THE NAVLYS SERIES, MODERATELY WET, CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS AND HIGH TERRACES. THE SURFACE LAYER IS MIXED BROWN AND YELLOWISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 9 INCHES AND YELLOWISH BROWN MOTTLED SILT LOAM IN LOWER 7 INCHES. THE SUBSTRATUM IS YELLOWISH BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 18 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND, AND WOODLAND."|"198890:279407"|"198890:171975"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Navlys component makes up 85 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills. The parent material consists of calcareous loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent."|"198890:279407"|"198890:1241823"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Birds component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198891:1568269"|"198891:1244141"
|"SOI5 description"|||"THE BIRDS SERIES DRAINED CONSISTS OF POORLY DRAINED SOILS FORMED UNDER FOREST VEGETATION IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE NEXT 16 INCHES IS GRAY MOTTLED SILT LOAM TRANSITIONAL LAYER. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198891:1568269"|"198891:1244140"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orion component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198891:289210"|"198891:1241936"
|"SOI5 description"|||"THE ORION SERIES CONSISTS OF DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 5 INCHES THICK. THE SUBSTRATUM IS 16 INCHES OF BROWN AND DARK GRAYISH BROWN MOTTLED SILT LOAM WITH THIN VERY FINE SAND STRATA OVER 21 INCHES OF BLACK AND VERY DARK GRAYISH BROWN MOTTLED SILT LOAM AND SILTY CLAY LOAM OVER DARK GRAYISH BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. AREAS ARE USED FOR PASTURELAND, WOODLAND AND CROPLAND."|"198891:289210"|"198891:185758"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198892:1568252"|"198892:1243966"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198892:1568252"|"198892:1243967"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198892:1568261"|"198892:1243986"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"198892:1568261"|"198892:1243985"
|"SOI5 description"|||"THE NAMEOKI SERIES, DRAINED, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN AND BROWN SILTY CLAY IN UPPER 16 INCHES AND DARK GRAYISH BROWN STRATIFIED CLAY LOAM, SILTY CLAY LOAM, SILT LOAM, AND LOAM IN LOWER 26 INCHES. THE SUBSTRATUM IS GRAYISH BROWN STRATIFIED SILT LOAM AND VERY FINE SANDY LOAM. REDOXIMORPHIC FEATURES ARE BELOW A DEPTH OF 12 INCHES. CROPLAND"|"198892:264402"|"198892:168516"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Nameoki component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over sandy and loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198892:264402"|"198892:1241939"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Water is a miscellaneous area."|"198893:284368"|"198893:1201208"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Littleton soil is a minor component."|"198895:1545910"|"198895:1181328"
|"SOI5 description"|||"THE LITTLETON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON TERRACES, ALLUVIAL FANS AND UPLAND TOE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAY AND VERY DARK GRAYISH BROWN SILT LOAM 26 INCHES THICK. THE SUBSOIL IS BROWN MOTTLED SILT LOAM 17 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198895:1545910"|"198895:1161924"
|"SOI5 description"|||"THE WORTHEN SERIES CONSISTS OF WELL DRAINED SOILS FORMED IN LOCAL ALLUVIUM ON FOOTSLOPES, TERRACES AND ALLUVIAL FANS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND DARK BROWN SILT LOAM 29 INCHES THICK. THE SUBSOIL IS BROWN AND DARK YELLOWISH BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 12 PERCENT. CROPLAND IS THE MAIN USE."|"198895:290165"|"198895:186522"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Worthen component makes up 95 percent of the map unit. Slopes are 2 to 5 percent. This component is on alluvial fans. The parent material consists of silty valley side alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198895:290165"|"198895:1181327"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"198897:264324"|"198897:168442"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on uplands, loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198897:264324"|"198897:1181184"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"198898:264325"|"198898:168443"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on uplands, loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198898:264325"|"198898:1181185"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"198899:265127"|"198899:169160"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 90 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198899:265127"|"198899:1241790"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"198900:265128"|"198900:169161"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 85 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198900:265128"|"198900:1241791"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"198901:265129"|"198901:169162"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 90 percent of the map unit. Slopes are 18 to 35 percent. This component is on uplands, loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198901:265129"|"198901:1181189"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198902:1169124"|"198902:824495"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Beaucoup soil is a minor component."|"198902:1169124"|"198902:1241898"
|"SOI5 description"|||"THE LITTLETON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON TERRACES, ALLUVIAL FANS AND UPLAND TOE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAY AND VERY DARK GRAYISH BROWN SILT LOAM 26 INCHES THICK. THE SUBSOIL IS BROWN MOTTLED SILT LOAM 17 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198902:289208"|"198902:185756"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Littleton component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on alluvial fans. The parent material consists of local silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198902:289208"|"198902:1241897"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Virden soil is a minor component."|"198903:1568245"|"198903:1243953"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198903:1568245"|"198903:1243952"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bethalto component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198903:265133"|"198903:1241794"
|"SOI5 description"|||"THE BETHALTO SERIES CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS UNDER MIXED PRAIRIE AND FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS DARK GRAYISH BROWN AND GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSOIL IS BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN UPPER 47 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. SLOPE RANGES FROM 0 TO 5 PERCENT. MOST AREAS ARE CROPPED."|"198903:265133"|"198903:169166"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Colp component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on lake plains. The parent material consists of thin loess over lacustrine deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 21 inches during January, February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198904:883360"|"198904:1241899"
|"SOI5 description"|||"THE COLP SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS OVER LACUSTRINE SEDIMENTS ON LACUSTRINE TERRACES, LAKE PLAINS, AND HIGH FLOOD PLAINS. THE SURFACE LAYER IS DARK BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 4 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND BROWN SILTY CLAY AND CLAY IN UPPER 36 INCHES AND LIGHT BROWNISH GRAY AND GRAYISH BROWN SILTY CLAY LOAM AND SILTY CLAY IN LOWER 32 INCHES. SLOPES RANGE FROM 1 TO 18 PERCENT. CROPLAND IS THE MAIN USE."|"198904:883360"|"198904:533886"
|"SOI5 description"|||"THE COLP SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS OVER LACUSTRINE SEDIMENTS ON LACUSTRINE TERRACES, LAKE PLAINS, AND HIGH FLOOD PLAINS. THE SURFACE LAYER IS DARK BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 4 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND BROWN SILTY CLAY AND CLAY IN UPPER 36 INCHES AND LIGHT BROWNISH GRAY AND GRAYISH BROWN SILTY CLAY LOAM AND SILTY CLAY IN LOWER 32 INCHES. SLOPES RANGE FROM 1 TO 18 PERCENT. CROPLAND IS THE MAIN USE."|"198905:883367"|"198905:533898"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Colp component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on lake plains. The parent material consists of lacustrine deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 21 inches during January, February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198905:883367"|"198905:1241900"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198906:1164861"|"198906:821454"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198906:1164861"|"198906:1241902"
|"SOI5 description"|||"THE ONARGA SERIES CONSISTS OF WELL AND MODERATELY WELL DRAINED SOILS FORMED IN SANDY SEDIMENTS ON OUTWASH PLAINS AND TERRACES. THE SURFACE LAYER IS VERY DARK BROWN FINE SANDY LOAM 16 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN, BROWN AND DARK YELLOWISH BROWN SANDY LOAM AND FINE SANDY LOAM 29 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN STRATIFIED LOAMY FINE SAND, FINE SAND AND FINE SANDY LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198906:280195"|"198906:172756"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Onarga component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on terraces. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2s.  This soil does not meet hydric criteria."|"198906:280195"|"198906:1241901"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198907:1321705"|"198907:937594"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Pierron soil is a minor component."|"198907:1321705"|"198907:1181209"
|"SOI5 description"|||"THE CASEYVILLE SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM AND BROWN SILTY CLAY LOAM 9 INCHES THICK. THE SUBSOIL IS BROWN SILTY CLAY LOAM IN UPPER 38 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. MOST AREAS ARE CROPPED."|"198907:265153"|"198907:169180"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Caseyville component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198907:265153"|"198907:1181208"
|"SOI5 description"|||"THE CASEYVILLE SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM AND BROWN SILTY CLAY LOAM 9 INCHES THICK. THE SUBSOIL IS BROWN SILTY CLAY LOAM IN UPPER 38 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. MOST AREAS ARE CROPPED."|"198908:265154"|"198908:169181"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Caseyville component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198908:265154"|"198908:1181210"
|"SOI5 description"|||"THE HURST SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLYING ACID, CLAYEY LAKEBED SEDIMENTS ON STREAM TERRACE. THE SURFACE LAYER IS DARK GRAYISH BROWN AND GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 6 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN, BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM AND SILTY CLAY 31 INCHES THICK. THE SUBSTRATUM IS LIGHT BROWNISH GRAY MOTTLED STRATIFIED SILTY CLAY LOAM AND SILTY CLAY. SLOPES RANGE FROM 0 TO 15 PERCENT. MOST AREA ARE USED FOR CROPLAND."|"198909:277577"|"198909:185577"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hurst component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on lake plains. The parent material consists of thin loess over lacustrine deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198909:277577"|"198909:1241905"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198910:265187"|"198910:169214"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 95 percent of the map unit. Slopes are 2 to 5 percent. This component is on loess hills, ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198910:265187"|"198910:1181247"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198911:289349"|"198911:185878"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 85 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of LOESS. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198911:289349"|"198911:1181246"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198912:265189"|"198912:169216"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 95 percent of the map unit. Slopes are 5 to 10 percent. This component is on loess hills, ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198912:265189"|"198912:1181248"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198913:265190"|"198913:169217"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198913:265190"|"198913:1241812"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"198914:265202"|"198914:1241817"
|"SOI5 description"|||"ORTHENTS, LOAMY, NONACID, CONSISTS OF WELL DRAINED AND MODERATELY WELL DRAINED SOILS FORMED IN NONACID DISTURBED SOIL MATERIAL. THE SURFACE LAYER IS DARK GRAYISH BROWN LOAM 6 INCHES THICK. THE SUBSTRATUM IS MIXED YELLOWISH BROWN AND BROWN LOAM AND SILT LOAM. SLOPES RANGE FROM 0 TO 50 PERCENT. MOST AREAS ARE USED FOR PASTURELAND."|"198915:1162003"|"198915:819911"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Orthents soil is a minor component."|"198915:1162003"|"198915:1201070"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Dumps is a miscellaneous area."|"198915:265203"|"198915:1241818"
|"SOI5 description"|||"ORTHENTS, SILTY CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORM IN DISTURBED, SILTY SOIL MATERIAL ON UPLANDS. THE SURFACE LAYER AND UNDERLYING MATERIAL IS MIXED BROWN AND GRAYISH BROWN, MOTTLED SILT LOAM AND SILTY CLAY LOAM TO A DEPTH OF 60 INCHES. SLOPES RANGE FROM 0 TO 35 PERCENT. MOST AREAS ARE IDLE OR ARE USED FOR LAWNS OR PARKWAYS."|"198916:265208"|"198916:169233"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents, Silty component makes up 85 percent of the map unit. Slopes are 0 to 5 percent.  The parent material consists of earthy fill. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.    This soil does not meet hydric criteria."|"198916:265208"|"198916:1241828"
|"SOI5 description"|||"ORTHENTS, SILTY CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORM IN DISTURBED, SILTY SOIL MATERIAL ON UPLANDS. THE SURFACE LAYER AND UNDERLYING MATERIAL IS MIXED BROWN AND GRAYISH BROWN, MOTTLED SILT LOAM AND SILTY CLAY LOAM TO A DEPTH OF 60 INCHES. SLOPES RANGE FROM 0 TO 35 PERCENT. MOST AREAS ARE IDLE OR ARE USED FOR LAWNS OR PARKWAYS."|"198917:265209"|"198917:169234"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents, Silty component makes up 85 percent of the map unit. Slopes are 5 to 35 percent.  The parent material consists of earthy fill. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.    This soil does not meet hydric criteria."|"198917:265209"|"198917:1241829"
|"SOI5 description"|||"ORTHENTS, LOAMY, NONACID, CONSISTS OF WELL DRAINED AND MODERATELY WELL DRAINED SOILS FORMED IN NONACID DISTURBED SOIL MATERIAL. THE SURFACE LAYER IS DARK GRAYISH BROWN LOAM 6 INCHES THICK. THE SUBSTRATUM IS MIXED YELLOWISH BROWN AND BROWN LOAM AND SILT LOAM. SLOPES RANGE FROM 0 TO 50 PERCENT. MOST AREAS ARE USED FOR PASTURELAND."|"198918:265211"|"198918:169236"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents, loamy component makes up 85 percent of the map unit. Slopes are 0 to 5 percent. This component is on cuts (road, railroad, etc.). The parent material consists of earthy fill. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 57 inches during February, March, April, May. Organic matter content in the surface horizon is about 1 percent.    This soil does not meet hydric criteria."|"198918:265211"|"198918:1201075"
|"SOI5 description"|||"ORTHENTS, LOAMY, NONACID, CONSISTS OF WELL DRAINED AND MODERATELY WELL DRAINED SOILS FORMED IN NONACID DISTURBED SOIL MATERIAL. THE SURFACE LAYER IS DARK GRAYISH BROWN LOAM 6 INCHES THICK. THE SUBSTRATUM IS MIXED YELLOWISH BROWN AND BROWN LOAM AND SILT LOAM. SLOPES RANGE FROM 0 TO 50 PERCENT. MOST AREAS ARE USED FOR PASTURELAND."|"198919:265212"|"198919:169237"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents, Loamy component makes up 85 percent of the map unit. Slopes are 5 to 35 percent.  The parent material consists of earthy fill. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 57 inches during January, February, March, April. Organic matter content in the surface horizon is about 1 percent.    This soil does not meet hydric criteria."|"198919:265212"|"198919:1241830"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Pits, quarries is a miscellaneous area."|"198920:264403"|"198920:1241831"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Pits, gravel is a miscellaneous area."|"198921:264849"|"198921:1241832"
|"SOI5 description"|||"THE SYLVAN SERIES, ERODED, CONSISTS OF WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS AND HIGH TERRACES. THE SURFACE LAYER IS BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND BROWN SILTY CLAY LOAM 19 INCHES THICK. THE SUBSTRATUM IS SILT LOAM THAT IS LIGHT BROWNISH GRAY IN THE UPPER PART AND MOTTLED LIGHT BROWNISH GRAY AND YELLOWISH BROWN IN THE LOWER PART. SLOPES RANGE FROM 2 TO 60 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198922:277575"|"198922:185575"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Sylvan component makes up 50 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 20 percent."|"198922:277575"|"198922:1181285"
|"SOI5 description"|||"THE BOLD SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS YELLOWISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN AND LIGHT GRAY SILT LOAM. SLOPES RANGE FROM 4 TO 75 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198922:277576"|"198922:185576"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bold component makes up 40 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills. The parent material consists of calcareous loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 30 percent."|"198922:277576"|"198922:1181286"
|"SOI5 description"|||"THE SYLVAN SERIES, ERODED, CONSISTS OF WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS AND HIGH TERRACES. THE SURFACE LAYER IS BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND BROWN SILTY CLAY LOAM 19 INCHES THICK. THE SUBSTRATUM IS SILT LOAM THAT IS LIGHT BROWNISH GRAY IN THE UPPER PART AND MOTTLED LIGHT BROWNISH GRAY AND YELLOWISH BROWN IN THE LOWER PART. SLOPES RANGE FROM 2 TO 60 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198923:265273"|"198923:169295"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Sylvan component makes up 50 percent of the map unit. Slopes are 18 to 35 percent. This component is on loess bluffs. The parent material consists of calcareous loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 20 percent."|"198923:265273"|"198923:1241836"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bold component makes up 40 percent of the map unit. Slopes are 18 to 35 percent.  The parent material consists of calcareous loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 30 percent."|"198923:265274"|"198923:1241837"
|"SOI5 description"|||"THE BOLD SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS YELLOWISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN AND LIGHT GRAY SILT LOAM. SLOPES RANGE FROM 4 TO 75 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198923:265274"|"198923:169296"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198924:1156738"|"198924:814906"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup, Undrained component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is very poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, June, July, August, September, October, November, December. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 5w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198924:1156738"|"198924:1241840"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198926:264258"|"198926:168392"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is frequently flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198926:264258"|"198926:1181301"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198927:276415"|"198927:174316"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on backswamps on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is frequently flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, June, November, December. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 5w.  This soil meets hydric criteria."|"198927:276415"|"198927:1181303"
|"SOI5 description"|||"THE DOCKERY SERIES, MODERATE PERM, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSTRATUM IS VERY DARK GRAYISH BROWN, GRAYISH BROWN AND VERY DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198928:1548202"|"198928:1181313"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Birds soil is a minor component."|"198928:1548202"|"198928:1174633"
|"SOI5 description"|||"THE SAWMILL SERIES, PONDED, CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED, SILTY CLAY LOAM 9 INCHES THICK. THE SUBSTRATUM IS OLIVE GRAY AND DARK GRAY, MOTTLED SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR WOODLAND."|"198928:1548300"|"198928:1181312"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Sawmill soil is a minor component."|"198928:1548300"|"198928:1174724"
|"SOI5 description"|||"THE WAKELAND SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS ON FLOOD PLAINS AND FLOODPLAIN STEPS. THEY FORMED IN SILTY ALLUVIUM. THE SURFACE LAYER IS GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM 53 INCHES THICK. DOMINANT USE IS CROPLAND."|"198928:265163"|"198928:169190"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Wakeland component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains, alluvial plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198928:265163"|"198928:1181311"
|"SOI5 description"|||"THE BIRDS SERIES DRAINED CONSISTS OF POORLY DRAINED SOILS FORMED UNDER FOREST VEGETATION IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE NEXT 16 INCHES IS GRAY MOTTLED SILT LOAM TRANSITIONAL LAYER. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198929:289636"|"198929:186134"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Birds component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is frequently flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 4w.  This soil meets hydric criteria."|"198929:289636"|"198929:1241886"
|"SOI5 description"|||"THE DOCKERY SERIES, MODERATE PERM, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSTRATUM IS VERY DARK GRAYISH BROWN, GRAYISH BROWN AND VERY DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198930:1550726"|"198930:1180409"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Birds soil is a minor component."|"198930:1550726"|"198930:1181315"
|"SOI5 description"|||"THE WILBUR SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS AND FLOOD-PLAIN STEPS. THE SURFACE LAYER IS BROWN SILT LOAM 7 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN AND BROWN MOTTLED SILT LOAM 25 INCHES THICK. THE SUBSTRATUM IS LIGHT BROWNISH GRAY MOTTLED SILT LOAM. CROPLAND IS THE DOMINANT USE."|"198930:264346"|"198930:168460"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Wilbur component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 21 inches during January, February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198930:264346"|"198930:1181314"
|"SOI5 description"|||"THE DOCKERY SERIES, MODERATE PERM, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSTRATUM IS VERY DARK GRAYISH BROWN, GRAYISH BROWN AND VERY DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198931:1568268"|"198931:1244020"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Birds soil is a minor component."|"198931:1568268"|"198931:1244021"
|"SOI5 description"|||"THE ORION SERIES CONSISTS OF DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 5 INCHES THICK. THE SUBSTRATUM IS 16 INCHES OF BROWN AND DARK GRAYISH BROWN MOTTLED SILT LOAM WITH THIN VERY FINE SAND STRATA OVER 21 INCHES OF BLACK AND VERY DARK GRAYISH BROWN MOTTLED SILT LOAM AND SILTY CLAY LOAM OVER DARK GRAYISH BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. AREAS ARE USED FOR PASTURELAND, WOODLAND AND CROPLAND."|"198931:265169"|"198931:169196"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orion component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil does not meet hydric criteria."|"198931:265169"|"198931:1241887"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Mascoutah component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198932:1568250"|"198932:1243963"
|"SOI5 description"|||"THE MASCOUTAH SERIES CONSISTS OF VERY DEEP POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BLACK AND VERY DARK GRAY SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY AND OLIVE GRAY SILTY CLAY LOAM IN THE UPPER 31 INCHES AND GRAY SILT LOAM IN THE LOWER 7 INCHES. THE SUBSTRATUM IS GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198932:1568250"|"198932:1243962"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Downsouth component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during January, February, March, April. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198932:265155"|"198932:1241798"
|"SOI5 description"|||"THE DOWNSOUTH SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS UNDER MIXED PRAIRIE AND FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS BROWN SILT LOAM 4 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN, YELLOWISH BROWN, AND BROWN SILTY CLAY LOAM IN UPPER 44 INCHES AND BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS PALE BROWN SILT LOAM. SLOPE RANGES FROM 2 TO 10 PERCENT. MOST AREAS ARE CROPPED."|"198932:265155"|"198932:169182"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Sawmill soil is a minor component."|"198933:1547538"|"198933:1172365"
|"SOI5 description"|||"THE SAWMILL SERIES, PONDED, CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED, SILTY CLAY LOAM 9 INCHES THICK. THE SUBSTRATUM IS OLIVE GRAY AND DARK GRAY, MOTTLED SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR WOODLAND."|"198933:1547538"|"198933:1181319"
|"SOI5 description"|||"THE DOCKERY SERIES, MODERATE PERM, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSTRATUM IS VERY DARK GRAYISH BROWN, GRAYISH BROWN AND VERY DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 5 PERCENT. CROPLAND IS THE MAIN USE."|"198933:1548203"|"198933:1181321"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Birds soil is a minor component."|"198933:1548203"|"198933:1174634"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Comfrey soil is a minor component."|"198933:1548213"|"198933:1174641"
|"SOI5 description"|||"THE COMFREY SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON BOTTOMLANDS. THE SURFACE SOIL IS BLACK CLAY LOAM 26 INCHES THICK. THE SUBSTRATUM IS DARK GRAY MOTTLED CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR PASTURELAND AND CROPLAND."|"198933:1548213"|"198933:1181317"
|"SOI5 description"|||"THE ZOOK SERIES CONSISTS OF POORLY DRAINED, FINE TEXTURED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS UNDER PRAIRIE VEGETATION. THE SURFACE SOIL IS BLACK SILTY CLAY LOAM AND VERY DARK GRAY SILTY CLAY 38 INCHES THICK. THE SUBSOIL IS VERY DARK GRAY AND DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSTRATUM IS DARK GRAY AND GRAY SILTY CLAY. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198933:1549827"|"198933:1176639"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Zook soil is a minor component."|"198933:1549827"|"198933:1181320"
|"SOI5 description"|||"THE OTTER SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE SOIL IS BLACK SILT LOAM 28 INCHES THICK. THE SUBSOIL IS DARK GRAYISH BROWN MOTTLED SILT LOAM 11 INCHES THICK. THE SUBSTRATUM IS DARK GRAY AND GRAY MOTTLED SILT LOAM AND LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198933:1550171"|"198933:1181318"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Otter soil is a minor component."|"198933:1550171"|"198933:1178359"
|"SOI5 description"|||"THE LAWSON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK BROWN SILT LOAM IN THE UPPER 12 INCHES AND BLACK AND VERY DARK BROWN SILT LOAM IN THE LOWER 18 INCHES. THE SUBSTRATUM IS 12 INCHES OF VERY DARK GRAY AND BLACK SILTY CLAY LOAM STRATIFIED WITH THIN LENSES OF SILT LOAM AND LOAM OVER DARK GRAYISH BROWN MOTTLED SILT LOAM INTERLAYED WITH THIN LENSES OF LOAM AND SANDY LOAM. SLOPES RANGE FROM 0 TO 3 PERCENT. AREAS ARE USED FOR PASTURELAND AND CROPLAND."|"198933:265017"|"198933:169065"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Lawson component makes up 92 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3w.  This soil does not meet hydric criteria."|"198933:265017"|"198933:1181316"
|"SOI5 description"|||"THE RADDLE SERIES CONSIST OF WELL DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 12 INCHES THICK. THE SILT LOAM SUBSOIL IS DARK BROWN IN THE UPPER 30 INCHES AND DARK YELLOWISH BROWN IN THE LOWER 18 INCHES. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS USED FOR CROPLAND."|"198934:264379"|"198934:168493"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Raddle component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on alluvial fans. The parent material consists of local silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198934:264379"|"198934:1241906"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198935:264384"|"198935:168498"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198935:264384"|"198935:1241917"
|"SOI5 description"|||"THE MASCOUTAH SERIES CONSISTS OF VERY DEEP POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BLACK AND VERY DARK GRAY SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY AND OLIVE GRAY SILTY CLAY LOAM IN THE UPPER 31 INCHES AND GRAY SILT LOAM IN THE LOWER 7 INCHES. THE SUBSTRATUM IS GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198936:1568249"|"198936:1243960"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Mascoutah component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198936:1568249"|"198936:1243961"
|"SOI5 description"|||"THE DOWNSOUTH SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS UNDER MIXED PRAIRIE AND FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS BROWN SILT LOAM 4 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN, YELLOWISH BROWN, AND BROWN SILTY CLAY LOAM IN UPPER 44 INCHES AND BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS PALE BROWN SILT LOAM. SLOPE RANGES FROM 2 TO 10 PERCENT. MOST AREAS ARE CROPPED."|"198936:265156"|"198936:169183"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Downsouth component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during January, February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198936:265156"|"198936:1241800"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Mascoutah component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198937:1568248"|"198937:1243959"
|"SOI5 description"|||"THE MASCOUTAH SERIES CONSISTS OF VERY DEEP POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BLACK AND VERY DARK GRAY SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY AND OLIVE GRAY SILTY CLAY LOAM IN THE UPPER 31 INCHES AND GRAY SILT LOAM IN THE LOWER 7 INCHES. THE SUBSTRATUM IS GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198937:1568248"|"198937:1243958"
|"SOI5 description"|||"THE EDWARDSVILLE SERIES CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAYISH BROWN. GRAYISH BROWN, AND LIGHT BROWNISH GRAY SILTY CLAY LOAM IN UPPER 34 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES IN THE SUBSOIL AND IN THE SUBSTRATUM. MOST AREAS ARE CROPPED."|"198937:265173"|"198937:734077"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Edwardsville component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198937:265173"|"198937:1241802"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Mascoutah component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198938:265175"|"198938:1241804"
|"SOI5 description"|||"THE MASCOUTAH SERIES CONSISTS OF VERY DEEP POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BLACK AND VERY DARK GRAY SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY AND OLIVE GRAY SILTY CLAY LOAM IN THE UPPER 31 INCHES AND GRAY SILT LOAM IN THE LOWER 7 INCHES. THE SUBSTRATUM IS GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE SOIL. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198938:265175"|"198938:169202"
|"SOI5 description"|||"THE ROCHER SERIES CONSISTS OF SOMEWHAT EXCESSIVELY DRAINED SOILS FORMED IN CALCAREOUS STRATIFIED ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS DARK BROWN LOAM 5 INCHES THICK. THE SUBSTRATUM IS STRATIFIED BROWN VERY FINE SANDY LOAM, LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAMY VERY FINE SAND AND LIGHT YELLOWISH BROWN LOAMY FINE SAND. SLOPES RANGE FROM 0 TO 7 PERCENT. CROPLAND IS THE MAIN USE."|"198939:265157"|"198939:169184"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Rocher component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on flood plains. The parent material consists of sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat excessively drained.  Water movement in the most restrictive layer is high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is frequently flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 3w.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 18 percent."|"198939:265157"|"198939:1241885"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"198940:264401"|"198940:168515"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198940:264401"|"198940:1241938"
|"SOI5 description"|||"THE BOLD SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS YELLOWISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN AND LIGHT GRAY SILT LOAM. SLOPES RANGE FROM 4 TO 75 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198941:277485"|"198941:185686"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bold component makes up 90 percent of the map unit. Slopes are 18 to 35 percent. This component is on loess bluffs. The parent material consists of calcareous loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 30 percent."|"198941:277485"|"198941:1241788"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198942:1568257"|"198942:1243976"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198942:1568257"|"198942:1243977"
|"SOI5 description"|||"THE OAKVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN FINE SAND SEDIMENTS ON OUTWASH AND LAKE PLAINS, MORAINES, AND BEACH RIDGES. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN FINE SAND 7 INCHES THICK. THE SUBSOIL IS STRONG BROWN, YELLOWISH BROWN AND BROWN FINE SAND 27 INCHES THICK. THE SUBSTRATUM IS PALE BROWN FINE SAND. SLOPES RANGE FROM 0 TO 60 PERCENT. MOST AREAS ARE IN WOODLAND OR IDLE CROPLAND."|"198942:277555"|"198942:185569"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oakville component makes up 85 percent of the map unit. Slopes are 2 to 5 percent. This component is on terraces. The parent material consists of eolian deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is high. Available water to a depth of 60 inches is low.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4s.  This soil does not meet hydric criteria."|"198942:277555"|"198942:1241911"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198943:1568256"|"198943:1243975"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198943:1568256"|"198943:1243974"
|"SOI5 description"|||"THE OAKVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN FINE SAND SEDIMENTS ON OUTWASH AND LAKE PLAINS, MORAINES, AND BEACH RIDGES. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN FINE SAND 7 INCHES THICK. THE SUBSOIL IS STRONG BROWN, YELLOWISH BROWN AND BROWN FINE SAND 27 INCHES THICK. THE SUBSTRATUM IS PALE BROWN FINE SAND. SLOPES RANGE FROM 0 TO 60 PERCENT. MOST AREAS ARE IN WOODLAND OR IDLE CROPLAND."|"198943:277557"|"198943:185570"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oakville component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on terraces. The parent material consists of eolian deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is high. Available water to a depth of 60 inches is low.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 6s.  This soil does not meet hydric criteria."|"198943:277557"|"198943:1241913"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 90 percent of the map unit. Slopes are 10 to 18 percent. This component is on loess hills, ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198944:913018"|"198944:567799"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198944:913018"|"198944:1181251"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bloomfield component makes up 85 percent of the map unit. Slopes are 2 to 5 percent. This component is on terraces. The parent material consists of eolian sands. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat excessively drained.  Water movement in the most restrictive layer is high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 3s.  This soil does not meet hydric criteria."|"198945:277481"|"198945:1241896"
|"SOI5 description"|||"THE BLOOMFIELD SERIES CONSISTS OF SOMEWHAT EXCESSIVELY DRAINED SOILS FORMED IN SANDY SEDIMENTS ON TERRACES AND UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN FINE SAND 5 INCHES THICK. THE SUBSURFACE LAYER IS BROWN AND YELLOWISH BROWN FINE SANDY 33 INCHES THICK. THE NEXT 20 INCHES IS YELLOWISH BROWN FINE SAND WITH DARK BROWN LOAMY FINE SAND BANDS. THE NEXT 22 INCHES IS DARK BROWN LOAMY FINE SAND WITH YELLOWISH BROWN FINE SAND INTERBANDS. THE SUBSTRATUM IS BROWN FINE SAND. SLOPES RANGE FROM 1 TO 50 PERCENT. MOST AREAS ARE USED FOR PASTURELAND OR WOODLAND."|"198945:277481"|"198945:185685"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198946:1568280"|"198946:1244345"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198946:1568280"|"198946:1244344"
|"SOI5 description"|||"THE HAYMOND SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN SILTY ALLUVIUM ON FLOODPLAINS AND FLOOD-PLAIN STEPS. THE SURFACE LAYER IS BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN AND YELLOWISH BROWN SILT LOAM 34 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN FINE SANDY LOAM. CROPLAND IS THE DOMINANT USE."|"198946:287119"|"198946:185691"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Haymond component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198946:287119"|"198946:1241931"
|"SOI5 description"|||"THE BIRDS SERIES DRAINED CONSISTS OF POORLY DRAINED SOILS FORMED UNDER FOREST VEGETATION IN SILTY ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE NEXT 16 INCHES IS GRAY MOTTLED SILT LOAM TRANSITIONAL LAYER. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198947:913026"|"198947:567812"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Birds component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198947:913026"|"198947:1241935"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Atlas soil is a minor component."|"198948:1540119"|"198948:1181161"
|"SOI5 description"|||"THE ATLAS SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN THIN LOESS AND GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY CLAY AND SILTY CLAY IN UPPER 34 INCHES AND AND LIGHT BROWNISH GRAY CLAY LOAM IN LOWER 33 INCHES. SLOPES RANGE FROM 2 TO 30 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198948:1540119"|"198948:1139330"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Homen soil is a minor component."|"198948:1540156"|"198948:1181162"
|"SOI5 description"|||"THE HOMEN SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS YELLOWISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 43 INCHES AND BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198948:1540156"|"198948:1139396"
|"SOI5 description"|||"THE GOSPORT SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN RESIDUUM WEATHERED FROM SHALE UNDER FOREST VEGETATION ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILTY CLAY 7 INCHES THICK. THE SUBSOIL IS BROWN, LIGHT OLIVE BROWN AND GRAYISH BROWN, FIRM AND EXTREMELY FIRM SILTY CLAY AND CLAY 20 INCHES THICK. THE SUBSTRATUM IS GRAY CLAY SHALE. SLOPES RANGE FROM 5 TO 50 PERCENT. WOODLAND AND PASTURELAND ARE THE MAIN USES."|"198948:1540163"|"198948:1181163"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Marseilles soil is a minor component."|"198948:1540163"|"198948:1139400"
|"SOI5 description"|||"THE ROZETTA SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 4 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSOIL IS BROWN, DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 39 INCHES THICK. THE SUBSTRATUM IS YELLOWISH BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 25 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"198948:1540178"|"198948:1181160"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Rozetta soil is a minor component."|"198948:1540178"|"198948:1139431"
|"SOI5 description"|||"THE HICKORY SERIES, ERODED, CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN GLACIAL TILL OR A THIN LAYER OF LOESS AND THE UNDERLYING GLACIAL TILL ON DISSECTED TILL PLAINS. THE SURFACE LAYER IS BROWN SILT LOAM 5 INCHES THICK. THE SUBSOIL IS BROWN AND YELLOWISH BROWN CLAY LOAM IN THE UPPER 34 INCHES AND YELLOWISH BROWN MOTTLED CLAY LOAM IN THE LOWER 12 INCHES. THE SUBSTRATUM IS YELLOWISH BROWN, MOTTLED LOAM. AREAS ARE USED FOR PASTURLAND, WOODLAND, AND CROPLAND"|"198948:280194"|"198948:172755"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hickory component makes up 91 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198948:280194"|"198948:1181159"
|"SOI5 description"|||"THE COULTERVILLE VARIANT CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLING SEDIMENTS ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM IN THE UPPER 27 INCHES AND GRAY MOTTLED SILT LOAM IN THE LOWER 21 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198949:1071581"|"198949:720892"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Burksville soil is a minor component."|"198949:1071581"|"198949:1240069"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Pierron component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on till plains. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198949:265118"|"198949:1209813"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198949:265118"|"198949:169151"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hickory component makes up 91 percent of the map unit. Slopes are 18 to 35 percent. This component is on ground moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198950:264314"|"198950:1120896"
|"SOI5 description"|||"THE HICKORY SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN GLACIAL TILL THAT CAN BE CAPPED WITH A THIN LAYER OF LOESS ON TILL PLAINS.THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK.THE SUBSURFACE LAYER IS LIGHT YELLOWISH BROWN SILT LOAM 8 INCHES THICK.THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN CLAY LOAM IN UPPER 34 INCHES AND LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAM IN LOWER 19 INCHES.THE SUBSTRATUM IS YELLOWISH BROWN, STRONG BROWN AND LIGHT GRAY LOAM."|"198950:264314"|"198950:905579"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198951:1540136"|"198951:1181174"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"198951:1540136"|"198951:1139380"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198951:1540169"|"198951:1181173"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Piasa soil is a minor component."|"198951:1540169"|"198951:1139423"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Virden soil is a minor component."|"198951:1540231"|"198951:1139471"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198951:1540231"|"198951:1181172"
|"SOI5 description"|||"THE HERRICK SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 11 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE MOTTLED SILTY CLAY LOAM SUBSOIL, 43 INCHES THICK, IS DARK GRAYISH BROWN IN UPPER PART, BROWN IN MIDDLE PART AND YELLOWISH BROWN IN LOWER PART. THE SUBSTRATUM IS YELLOWISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198951:265121"|"198951:1181171"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Herrick component makes up 92 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198951:265121"|"198951:169154"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198952:265122"|"198952:169155"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Virden component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198952:265122"|"198952:1181175"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"198953:1540135"|"198953:1240305"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198953:1540135"|"198953:1139378"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198953:1540168"|"198953:1240306"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Piasa soil is a minor component."|"198953:1540168"|"198953:1139406"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oconee component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198953:265138"|"198953:169171"
|"SOI5 description"|||"THE OCONEE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM AND SILTY CLAY 42 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 7 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198953:265138"|"198953:1240304"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Elco component makes up 95 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess over paleosol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198954:286873"|"198954:1181202"
|"SOI5 description"|||"THE ELCO SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS AND THE UNDERLYING PALEOSOL ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE SUBSURFACE IS BROWN SILT LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILT LOAM AND SILTY CLAY LOAM IN UPPER 14 INCHES, MIXED GRAYISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM AND CLAY LOAM IN NEXT 29 INCHES AND MOTTLED GRAY LOAM IN LOWER 15 INCHES. SLOPES RANGE FROM 2 TO 25 PERCENT. AREAS ARE USED FOR CROPLAND. PASTURELAND AND WOODLAND."|"198954:286873"|"198954:185689"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Elco component makes up 95 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess over paleosol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198955:288707"|"198955:1181198"
|"SOI5 description"|||"THE ELCO SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS AND THE UNDERLYING PALEOSOL ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE SUBSURFACE IS BROWN SILT LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILT LOAM AND SILTY CLAY LOAM IN UPPER 14 INCHES, MIXED GRAYISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM AND CLAY LOAM IN NEXT 29 INCHES AND MOTTLED GRAY LOAM IN LOWER 15 INCHES. SLOPES RANGE FROM 2 TO 25 PERCENT. AREAS ARE USED FOR CROPLAND. PASTURELAND AND WOODLAND."|"198955:288707"|"198955:185626"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Elco component makes up 94 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess over palesol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198956:912959"|"198956:1241796"
|"SOI5 description"|||"THE ELCO SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS AND THE UNDERLYING PALEOSOL ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE SUBSURFACE IS BROWN SILT LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILT LOAM AND SILTY CLAY LOAM IN UPPER 14 INCHES, MIXED GRAYISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM AND CLAY LOAM IN NEXT 29 INCHES AND MOTTLED GRAY LOAM IN LOWER 15 INCHES. SLOPES RANGE FROM 2 TO 25 PERCENT. AREAS ARE USED FOR CROPLAND. PASTURELAND AND WOODLAND."|"198956:912959"|"198956:567748"
|"SOI5 description"|||"THE WEIR SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 9 INCHES THICK. THE SUBSOIL IS GRAY MOTTLED SILTY CLAY LOAM IN UPPER 22 INCHES AND LIGHT GRAY MOTTLED SILT LOAM IN LOWER 7 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198957:289209"|"198957:185757"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Weir component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of LOESS. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198957:289209"|"198957:1241797"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Pierron soil is a minor component."|"198958:1541310"|"198958:1142680"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198958:1541310"|"198958:1240086"
|"SOI5 description"|||"THE MARINE SERIES CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR IN LOESS AND GLACIAL DRIFT ON INTERFLUVS CONVEX SUMMITS OF TILL PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN MOTTLED SILTY CLAY AND SILTY CLAY LOAM IN UPPER 17 INCHES, GRAYISH BROWN, MOTTLED SILTY CLAY LOAM IN THE NEXT 9 INCHES, AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM AND SILT LOAM IN LOWER 17 IN. THE SUBSTRATUM IS MOTTLED BROWN SILT LOAM. CROPLAND IS MAIN USE."|"198958:265201"|"198958:169228"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Marine component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on -- Error in Exists On --. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198958:265201"|"198958:1209853"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Rushville soil is a minor component."|"198959:1071557"|"198959:1240085"
|"SOI5 description"|||"THE RUSHVILLE SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY SILTY CLAY AND SILTY CLAY LOAM 37 INCHES THICK. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. REDOXIMORPHIC FEATURES ARE THROUGHOUT THE PROFILE. CROPLAND IS MAIN USE."|"198959:1071557"|"198959:720865"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Pierron soil is a minor component."|"198959:1541309"|"198959:1240084"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198959:1541309"|"198959:1142679"
|"SOI5 description"|||"THE MARINE SERIES CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR IN LOESS AND GLACIAL DRIFT ON INTERFLUVS CONVEX SUMMITS OF TILL PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN MOTTLED SILTY CLAY AND SILTY CLAY LOAM IN UPPER 17 INCHES, GRAYISH BROWN, MOTTLED SILTY CLAY LOAM IN THE NEXT 9 INCHES, AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM AND SILT LOAM IN LOWER 17 IN. THE SUBSTRATUM IS MOTTLED BROWN SILT LOAM. CROPLAND IS MAIN USE."|"198959:265200"|"198959:169227"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Marine component makes up 95 percent of the map unit. Slopes are 0 to 2 percent. This component is on -- Error in Exists On --. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198959:265200"|"198959:1209852"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198960:1568247"|"198960:1243956"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"198960:1568247"|"198960:1243957"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Burksville component makes up 93 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198960:1568285"|"198960:1244355"
|"SOI5 description"|||"THE COULTERVILLE VARIANT CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLING SEDIMENTS ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM IN THE UPPER 27 INCHES AND GRAY MOTTLED SILT LOAM IN THE LOWER 21 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198960:1568285"|"198960:1244354"
|"SOI5 description"|||"THE TAMALCO SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS AND UNDERLYING LOAMY DEPOSITS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE IS BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS BROWN AND REDDISH BROWN SILTY CLAY LOAM AND SILTY CLAY IN UPPER 8 INCHES, PALE BROWN MOTTLED SILTY CLAY LOAM IN NEXT 11 INCHES, GRAY AND LIGHT BROWNISH GRAY MOTTLED SILT LOAM IN LOWER 14 INCHES. THE SUBSTRATUM IS GRAYISH BROWN AND DARK BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 7 PERCENT. CROPLAND AND PASTURELAND ARE THE MAIN USES."|"198960:287007"|"198960:185690"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Tamalco component makes up 85 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 45 inches during March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. The soil has a slightly saline horizon within 30 inches of the soil surface. The soil has a moderately sodic horizon within 30 inches of the soil surface."|"198960:287007"|"198960:1241819"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Negley component makes up 85 percent of the map unit. Slopes are 18 to 35 percent. This component is on crevasse fillings. The parent material consists of outwash. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198961:265207"|"198961:1241822"
|"SOI5 description"|||"THE NEGLEY SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN OUTWASH SEDIMENTS ON KAMES, ESKERS AND TERRACES. THE SURFACE LAYER IS BROWN LOAM 8 INCHES THICK. THE SUBSOIL IS STRONG BROWN AND BROWN LOAM IN UPPER 16 INCHES, YELLOWISH RED AND REDDISH BROWN GRAVELLY CLAY LOAM, GRAVELLY SANDY CLAY LOAM, SANDY CLAY LOAM AND SANDY CLAY IN NEXT 68 INCHES AND YELLOWISH BROWN COARSE SANDY LOAM IN LOWER 7 INCHES. SLOPES RANGE FROM 2 TO 70 PERCENT. AREAS ARE USED FOR PASTURELAND, CROPLAND AND WOODLAND."|"198961:265207"|"198961:169232"
|"SOI5 description"|||"THE HOMEN SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS YELLOWISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 43 INCHES AND BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198962:265206"|"198962:1212325"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Homen component makes up 90 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198962:265206"|"198962:169231"
|"SOI5 description"|||"THE HOMEN SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS YELLOWISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 43 INCHES AND BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198963:265204"|"198963:169229"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Homen component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on uplands, -- Error in Exists On --. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198963:265204"|"198963:1181257"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"198964:1567527"|"198964:1239943"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Pierron soil is a minor component."|"198964:1567527"|"198964:1240092"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Burksville component makes up 93 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198964:264377"|"198964:1209865"
|"SOI5 description"|||"THE COULTERVILLE VARIANT CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLING SEDIMENTS ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM IN THE UPPER 27 INCHES AND GRAY MOTTLED SILT LOAM IN THE LOWER 21 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198964:264377"|"198964:168491"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ruma component makes up 85 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198965:265193"|"198965:1241816"
|"SOI5 description"|||"THE RUMA SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 35 INCHES AND YELLOWISH BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198965:265193"|"198965:169220"
|"SOI5 description"|||"THE RUMA SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 35 INCHES AND YELLOWISH BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198966:277579"|"198966:185578"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ruma component makes up 85 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of LOESS OVER SILTY PEDISEDIMENT. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198966:277579"|"198966:1241815"
|"SOI5 description"|||"THE RUMA SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 35 INCHES AND YELLOWISH BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198967:264359"|"198967:168473"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ruma component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198967:264359"|"198967:1241814"
|"SOI5 description"|||"THE RUMA SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 35 INCHES AND YELLOWISH BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"198968:264358"|"198968:168472"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ruma component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198968:264358"|"198968:1241813"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bunkum component makes up 90 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198969:265199"|"198969:169226"
|"SOI5 description"|||"THE BUNKUM SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN UPPER 24 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. MOST AREAS ARE CROPPED."|"198969:265199"|"198969:1240083"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bunkum component makes up 90 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines, uplands. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198970:265198"|"198970:169225"
|"SOI5 description"|||"THE BUNKUM SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN UPPER 24 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. MOST AREAS ARE CROPPED."|"198970:265198"|"198970:1181254"
|"SOI5 description"|||"THE BUNKUM SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN UPPER 24 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. MOST AREAS ARE CROPPED."|"198971:281928"|"198971:174399"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bunkum component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"198971:281928"|"198971:1240082"
|"SOI5 description"|||"THE COULTERVILLE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR IN LOESS AND LOAMY MATERIAL ON TILL PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE MOTTLED SUBSOIL IS BROWN AND GRAY SILTY CLAY LOAM IN UPPER 16 INCHES AND GRAY, LIGHT OLIVE GRAY, OLIVE AND BROWN SILT LOAM IN LOWER 33 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198972:265249"|"198972:1240098"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Coulterville component makes up 45 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198972:265249"|"198972:169271"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darmstadt component makes up 45 percent of the map unit. Slopes are 2 to 5 percent.  The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  The soil has a moderately sodic horizon within 30 inches of the soil surface."|"198972:265250"|"198972:169272"
|"SOI5 description"|||"THE DARMSTADT SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR LOESS AND LOAMY SEDIMENTS ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY AND GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS BROWN, PALE BROWN, LIGHT BROWNISH GRAY AND LIGHT GRAY MOTTLED SILTY CLAY LOAM 28 INCHES THICK. THE SUBSTRATUM IS LIGHT GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198972:265250"|"198972:1240099"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Coulterville component makes up 50 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198973:265247"|"198973:169269"
|"SOI5 description"|||"THE COULTERVILLE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR IN LOESS AND LOAMY MATERIAL ON TILL PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE MOTTLED SUBSOIL IS BROWN AND GRAY SILTY CLAY LOAM IN UPPER 16 INCHES AND GRAY, LIGHT OLIVE GRAY, OLIVE AND BROWN SILT LOAM IN LOWER 33 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198973:265247"|"198973:1209905"
|"SOI5 description"|||"THE GRANTFORK SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOAMY SEDIMENTS AND THE UNDERLYING GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY LOAM IN UPPER 32 INCHES AND LIGHT BROWNISH GRAY CLAY LOAM AND LOAM IN LOWER 27 INCHES. SLOPES RANGE FROM 2 TO 20 PERCENT. PASTURELAND AND HAYLAND ARE THE MAIN USES."|"198973:265248"|"198973:1209906"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Grantfork component makes up 40 percent of the map unit. Slopes are 5 to 10 percent.  The parent material consists of loess over loamy pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198973:265248"|"198973:169270"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Burksville soil is a minor component."|"198974:1567516"|"198974:1239720"
|"SOI5 description"|||"THE COULTERVILLE VARIANT CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLING SEDIMENTS ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM IN THE UPPER 27 INCHES AND GRAY MOTTLED SILT LOAM IN THE LOWER 21 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:1567516"|"198974:1240100"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:1567523"|"198974:1239814"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"198974:1567523"|"198974:1239815"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Piasa soil is a minor component."|"198974:1567524"|"198974:1239817"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:1567524"|"198974:1239816"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oconee component makes up 35 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198974:265255"|"198974:169277"
|"SOI5 description"|||"THE OCONEE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM AND SILTY CLAY 42 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 7 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:265255"|"198974:1209914"
|"SOI5 description"|||"THE COULTERVILLE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR IN LOESS AND LOAMY MATERIAL ON TILL PLAINS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE MOTTLED SUBSOIL IS BROWN AND GRAY SILTY CLAY LOAM IN UPPER 16 INCHES AND GRAY, LIGHT OLIVE GRAY, OLIVE AND BROWN SILT LOAM IN LOWER 33 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:265256"|"198974:169278"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Coulterville component makes up 30 percent of the map unit. Slopes are 2 to 5 percent.  The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198974:265256"|"198974:1209915"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darmstadt component makes up 20 percent of the map unit. Slopes are 2 to 5 percent.  The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent. The soil has a very slightly saline horizon within 30 inches of the soil surface. The soil has a moderately sodic horizon within 30 inches of the soil surface."|"198974:265257"|"198974:169279"
|"SOI5 description"|||"THE DARMSTADT SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS OR LOESS AND LOAMY SEDIMENTS ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY AND GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS BROWN, PALE BROWN, LIGHT BROWNISH GRAY AND LIGHT GRAY MOTTLED SILTY CLAY LOAM 28 INCHES THICK. THE SUBSTRATUM IS LIGHT GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 10 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198974:265257"|"198974:1209916"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Bunkum component makes up 55 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198975:265267"|"198975:169289"
|"SOI5 description"|||"THE BUNKUM SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 8 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN UPPER 24 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. MOST AREAS ARE CROPPED."|"198975:265267"|"198975:1240105"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Atlas component makes up 35 percent of the map unit. Slopes are 10 to 18 percent.  The parent material consists of loess over paleosol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198975:265268"|"198975:169290"
|"SOI5 description"|||"THE ATLAS SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN THIN LOESS AND GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY CLAY AND SILTY CLAY IN UPPER 34 INCHES AND AND LIGHT BROWNISH GRAY CLAY LOAM IN LOWER 33 INCHES. SLOPES RANGE FROM 2 TO 30 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198975:265268"|"198975:1240106"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Herrick component makes up 45 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198976:265264"|"198976:1181280"
|"SOI5 description"|||"THE HERRICK SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 11 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK. THE MOTTLED SILTY CLAY LOAM SUBSOIL, 43 INCHES THICK, IS DARK GRAYISH BROWN IN UPPER PART, BROWN IN MIDDLE PART AND YELLOWISH BROWN IN LOWER PART. THE SUBSTRATUM IS YELLOWISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198976:265264"|"198976:169286"
|"SOI5 description"|||"THE BIDDLE SERIES, DRAINED, CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 13 INCHES THICK. THE SUBSURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS BROWN AND GRAYISH BROWN SILTY CLAY LOAM IN THE UPPER 39 INCHES AND GRAYISH BROWN SILT LOAM IN THE LOWER 7 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. MOST AREAS ARE CROPPED."|"198976:265265"|"198976:1181281"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Biddle component makes up 30 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 8 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198976:265265"|"198976:169287"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198976:265266"|"198976:169288"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Piasa component makes up 20 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines, depressions. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. The soil has a very slightly saline horizon within 30 inches of the soil surface. The soil has a moderately sodic horizon within 30 inches of the soil surface."|"198976:265266"|"198976:1181282"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Virden component makes up 50 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria."|"198977:265260"|"198977:1181278"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198977:265260"|"198977:169282"
|"SOI5 description"|||"THE FOSTERBURG SERIES, DRAINED, CONSISTS OF VERY DEEP POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS BLACK SILT LOAM 13 INCHES THICK. THE SUBSOIL IS VERY DARK GRAY, DARK GRAY, AND GRAYISH BROWN SILTY CLAY LOAM IN THE UPPER 49 INCHES AND OLIVE GRAY SILT LOAM IN THE LOWER 9 INCHES. THE SUBSTRATUM IS LIGHT OLIVE GRAY SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES IN THE SUBSOIL AND IN THE SUBSTRATUM. MOST AREAS ARE CROPPED."|"198977:265261"|"198977:169283"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fosterburg component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on depressions. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198977:265261"|"198977:1181279"
|"SOI5 description"|||"THE ATLAS SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN THIN LOESS AND GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY CLAY AND SILTY CLAY IN UPPER 34 INCHES AND AND LIGHT BROWNISH GRAY CLAY LOAM IN LOWER 33 INCHES. SLOPES RANGE FROM 2 TO 30 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198978:288917"|"198978:185627"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Atlas component makes up 55 percent of the map unit. Slopes are 10 to 18 percent. This component is on ground moraines. The parent material consists of loess or silty pedisediment over till with a paleosol. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 12 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198978:288917"|"198978:1241834"
|"SOI5 description"|||"THE GRANTFORK SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOAMY SEDIMENTS AND THE UNDERLYING GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY LOAM IN UPPER 32 INCHES AND LIGHT BROWNISH GRAY CLAY LOAM AND LOAM IN LOWER 27 INCHES. SLOPES RANGE FROM 2 TO 20 PERCENT. PASTURELAND AND HAYLAND ARE THE MAIN USES."|"198978:288919"|"198978:185629"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Grantfork component makes up 35 percent of the map unit. Slopes are 10 to 18 percent.  The parent material consists of loamy pedisediment over till or till with a paleosol. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198978:288919"|"198978:1241835"
|"SOI5 description"|||"THE GRANTFORK SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOAMY SEDIMENTS AND THE UNDERLYING GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY LOAM IN UPPER 32 INCHES AND LIGHT BROWNISH GRAY CLAY LOAM AND LOAM IN LOWER 27 INCHES. SLOPES RANGE FROM 2 TO 20 PERCENT. PASTURELAND AND HAYLAND ARE THE MAIN USES."|"198979:288918"|"198979:185628"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Grantfork component makes up 35 percent of the map unit. Slopes are 5 to 10 percent.  The parent material consists of loamy pedisediment over till or paleosol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 15 percent.  The soil has a slightly sodic horizon within 30 inches of the soil surface."|"198979:288918"|"198979:1240108"
|"SOI5 description"|||"THE ATLAS SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN THIN LOESS AND GLACIAL TILL ON UPLANDS. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY CLAY AND SILTY CLAY IN UPPER 34 INCHES AND AND LIGHT BROWNISH GRAY CLAY LOAM IN LOWER 33 INCHES. SLOPES RANGE FROM 2 TO 30 PERCENT. MOST AREAS ARE USED FOR HAYLAND AND PASTURELAND."|"198979:288920"|"198979:185630"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Atlas component makes up 55 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess over paleosol formed in till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"198979:288920"|"198979:1240107"
|"SOI5 description"|||"THE GOSPORT SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN RESIDUUM WEATHERED FROM SHALE UNDER FOREST VEGETATION ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 4 INCHES THICK. THE SUBSURFACE LAYER IS GRAYISH BROWN SILTY CLAY LOAM 3 INCHES THICK. THE SUBSOIL IS BROWN, LIGHT OLIVE BROWN AND GRAYISH BROWN, FIRM AND EXTREMELY FIRM SILTY CLAY AND CLAY 20 INCHES THICK. THE SUBSTRATUM IS GRAY CLAY SHALE. SLOPES RANGE FROM 5 TO 50 PERCENT. WOODLAND AND PASTURELAND ARE THE MAIN USES."|"198980:277649"|"198980:185687"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Gosport component makes up 40 percent of the map unit. Slopes are 18 to 35 percent.  The parent material consists of residuum. Depth to a root restrictive layer, bedrock (paralithic), is 20 to 40 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is low. Available water to a depth of 60 inches is low.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria."|"198980:277649"|"198980:1241839"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hickory component makes up 50 percent of the map unit. Slopes are 18 to 35 percent. This component is on ground moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"198980:277650"|"198980:1241838"
|"SOI5 description"|||"THE HICKORY SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN GLACIAL TILL THAT CAN BE CAPPED WITH A THIN LAYER OF LOESS ON TILL PLAINS.THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK.THE SUBSURFACE LAYER IS LIGHT YELLOWISH BROWN SILT LOAM 8 INCHES THICK.THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN CLAY LOAM IN UPPER 34 INCHES AND LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAM IN LOWER 19 INCHES.THE SUBSTRATUM IS YELLOWISH BROWN, STRONG BROWN AND LIGHT GRAY LOAM."|"198980:277650"|"198980:185688"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Cowden component makes up 45 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"198981:265277"|"198981:169299"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198981:265277"|"198981:1181299"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198981:265278"|"198981:1181300"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Piasa component makes up 45 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. The soil has a very slightly saline horizon within 30 inches of the soil surface. The soil has a moderately sodic horizon within 30 inches of the soil surface."|"198981:265278"|"198981:169300"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is frequently flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, June, November, December. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 4w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"198982:265158"|"198982:169185"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198982:265158"|"198982:1181302"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Sawmill soil is a minor component."|"198983:1567529"|"198983:1239945"
|"SOI5 description"|||"THE SAWMILL SERIES, PONDED, CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED, SILTY CLAY LOAM 9 INCHES THICK. THE SUBSTRATUM IS OLIVE GRAY AND DARK GRAY, MOTTLED SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR WOODLAND."|"198983:1567529"|"198983:1239946"
|"SOI5 description"|||"THE COFFEEN SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS, LOW TERRACES AND FOOTSLOPES. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 12 INCHES THICK. THE SILT LOAM SUBSOIL IS DARK GRAYISH BROWN IN UPPER 7 INCHES, GRAYISH BROWN MOTTLED IN NEXT 5 INCHES AND LAYERED LIGHT BROWNISH GRAY, YELLOWISH BROWN AND BROWN IN LOWER 12 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY AND PALE BROWN STRATIFIED SILT LOAM AND LOAM. SLOPES ARE 0 TO 3 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"198983:265170"|"198983:169197"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Coffeen component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil does not meet hydric criteria."|"198983:265170"|"198983:1240112"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198984:1568251"|"198984:1243964"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198984:1568251"|"198984:1243965"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ridgeville component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on terraces. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 24 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2s.  This soil does not meet hydric criteria."|"198984:277545"|"198984:1241903"
|"SOI5 description"|||"THE RIDGEVILLE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON OUTWASH PLAINS AND STREAM TERRACES. THE SURFACE SOIL IS VERY DARK BROWN, VERY DARK GRAY AND DARK GRAYISH BROWN FINE SANDY LOAM 20 INCHES THICK. THE SUBSOIL IS DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SANDY LOAM AND SANDY CLAY LOAM IN UPPER 20 INCHES AND YELLOWISH BROWN MOTTLED LOAMY SAND IN LOWER 7 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY MOTTLED FINE SAND. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198984:277545"|"198984:185563"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"198985:1568258"|"198985:1243979"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"198985:1568258"|"198985:1243978"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Newhaven component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on terraces. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 24 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 1.  This soil does not meet hydric criteria."|"198985:277581"|"198985:1241909"
|"SOI5 description"|||"THE NEWHAVEN SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN OUTWASH ON STREAM TERRACES AND LAKE PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN LOAM 15 INCHES THICK. THE SUBSOIL IS DARK BROWN AND GRAYISH BROWN LOAM AND CLAY LOAM IN THE UPPER 25 INCHES, DARK BROWN SANDY LOAM IN THE NEXT 7 INCHES, AND YELLOWISH BROWN LOAMY SAND WITH DARK BROWN LAMELLA IN THE LOWER 33 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE CULTIVATED."|"198985:277581"|"198985:185579"
|"SOI5 description"|||"THE RIDGWAY SERIES CONSISTS OF WELL DRAINED SOILS FORMED IN LOESS AND LOAMY OR SANDY OUTWASH ON LOW TERRACES AND HIGH FLOODPLAINS. THE SURFACE LAEYR IS BROWN SITL LOAM 8 INCHES THICK. THE UPPER 19 INCHES OF THE SUBSOIL IS DARK YELLOWISH BROWN SILTY CLAY LOAM. THE NEXT 25 INCHES OF THE SUBSOIL IS BROWN CLAY LOAM AND FINE SANDY LOAM. THE LOWER PART OF THE SUBSOIL IS BANDED YELLOWISH BROWN FINE SAND AND BROWN LOAMY FINE SAND. SLOPES ARE 0 TO 10 PERCENT. AREAS ARE USED FOR CROPLAND."|"198986:883374"|"198986:533906"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ridgway component makes up 85 percent of the map unit. Slopes are 2 to 5 percent. This component is on stream terraces. The parent material consists of loess over outwash. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"198986:883374"|"198986:1241908"
|"SOI5 description"|||"THE GEFF SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN 24 TO 40 INCHES OF LOESS OR SILTY MATERIAL AND LOAMY OUTWASH ON FLOOD PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN AND BROWN SILT LOAM 12 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN MOTTLED SILT LOAM AND SILTY CLAY LOAM IN THE UPPER 20 INCHES, DARK YELLOWISH BROWN MOTTLED SILT LOAM AND LOAM IN THE NEXT 27 INCHES, AND YELLOWISH BROWN SAND WITH DARK BROWN LOAMY SAND LAMELLA IN THE LOWER 20 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. AREAS ARE USED MAINLY FOR CROPLAND."|"198987:883372"|"198987:533904"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Geff component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on stream terraces. The parent material consists of loess over outwash. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198987:883372"|"198987:1241907"
|"SOI5 description"|||"THE RADDLE SERIES CONSIST OF WELL DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILT LOAM 12 INCHES THICK. THE SILT LOAM SUBSOIL IS DARK BROWN IN THE UPPER 30 INCHES AND DARK YELLOWISH BROWN IN THE LOWER 18 INCHES. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS USED FOR CROPLAND."|"198989:280198"|"198989:172759"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Dozaville component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"198989:280198"|"198989:1241942"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200796:1550727"|"200796:1181245"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Virden soil is a minor component."|"200796:1550727"|"200796:1180410"
|"SOI5 description"|||"THE AVISTON SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILT LOAM 10 INCHES THICK. THE SUBSURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS BROWN SILTY CLAY LOAM IN THE UPPER 32 INCHES AND BROWN SILT LOAM IN THE LOWER 32 INCHES. THE SOIL CONTAINS REDOXIMORPHIC FEATURES BELOW A DEPTH OF 23 INCHES. MOST AREAS ARE CROPPED."|"200796:265181"|"200796:169208"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Aviston component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"200796:265181"|"200796:1181244"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200801:1568246"|"200801:1243954"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Virden soil is a minor component."|"200801:1568246"|"200801:1243955"
|"SOI5 description"|||"THE AVISTON SERIES CONSISTS OF VERY DEEP MODERATELY WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILT LOAM 10 INCHES THICK. THE SUBSURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS BROWN SILTY CLAY LOAM IN THE UPPER 32 INCHES AND BROWN SILT LOAM IN THE LOWER 32 INCHES. THE SOIL CONTAINS REDOXIMORPHIC FEATURES BELOW A DEPTH OF 23 INCHES. MOST AREAS ARE CROPPED."|"200801:265182"|"200801:169209"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Aviston component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"200801:265182"|"200801:1241805"
|"SOI5 description"|||"THE WAKENDA SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 14 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 37 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 9 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200802:265183"|"200802:169210"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Wakenda component makes up 90 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"200802:265183"|"200802:1241807"
|"SOI5 description"|||"THE WAKENDA SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 14 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 37 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 9 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200805:265184"|"200805:169211"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Wakenda component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3e.  This soil does not meet hydric criteria."|"200805:265184"|"200805:1241808"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"200824:1540141"|"200824:1241810"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200824:1540141"|"200824:1139384"
|"SOI5 description"|||"THE VIRDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS BLACK SILT LOAM 12 INCHES THICK. THE SUBSOIL IS BLACK, VERY DARK GRAY AND LIGHT OLIVE GRAY SILTY CLAY LOAM 41 INCHES THICK. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200824:1540232"|"200824:1139472"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Virden soil is a minor component."|"200824:1540232"|"200824:1241811"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200824:276397"|"200824:174304"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Piasa component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. The soil has a very slightly saline horizon within 30 inches of the soil surface. The soil has a moderately sodic horizon within 30 inches of the soil surface."|"200824:276397"|"200824:1241809"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"200826:265141"|"200826:169174"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is occasionally flooded. It is occasionally ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, November, December. Organic matter content in the surface horizon is about 4 percent.    This soil meets hydric criteria."|"200826:265141"|"200826:1241841"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200826:265142"|"200826:1241843"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Aquents component makes up 30 percent of the map unit. Slopes are 0 to 2 percent. This component is on fills, cuts (road, railroad, etc.).  Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is occasionally flooded. It is occasionally ponded. A seasonal zone of water saturation is at 0 inches during January, February, March, April, May, June, July, August, September, October, November, December.     This soil meets hydric criteria."|"200826:290101"|"200826:1241842"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"200827:265143"|"200827:169175"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 40 percent of the map unit. Slopes are 8 to 15 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.    This soil does not meet hydric criteria."|"200827:265143"|"200827:1241844"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200827:265144"|"200827:1241846"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Orthents is a miscellaneous area."|"200827:290102"|"200827:1241845"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Colp component makes up 40 percent of the map unit. Slopes are 2 to 5 percent. This component is on lake plains. The parent material consists of thin loess over lacustrine deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 21 inches during January, February, March, April. Organic matter content in the surface horizon is about 2 percent.    This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"200829:276473"|"200829:1241852"
|"SOI5 description"|||"THE COLP SERIES CONSISTS OF MODERATELY WELL DRAINED SOILS FORMED IN LOESS OVER LACUSTRINE SEDIMENTS ON LACUSTRINE TERRACES, LAKE PLAINS, AND HIGH FLOOD PLAINS. THE SURFACE LAYER IS DARK BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT BROWNISH GRAY SILT LOAM 4 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND BROWN SILTY CLAY AND CLAY IN UPPER 36 INCHES AND LIGHT BROWNISH GRAY AND GRAYISH BROWN SILTY CLAY LOAM AND SILTY CLAY IN LOWER 32 INCHES. SLOPES RANGE FROM 1 TO 18 PERCENT. CROPLAND IS THE MAIN USE."|"200829:276473"|"200829:158799"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents component makes up 30 percent of the map unit. Slopes are 2 to 5 percent.   Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches.     This soil does not meet hydric criteria."|"200829:290098"|"200829:1241853"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban Land is a miscellaneous area."|"200829:290099"|"200829:1241854"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fluvents component makes up 30 percent of the map unit. Slopes are 0 to 2 percent.  The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during March, April, May, June.     This soil does not meet hydric criteria."|"200830:1156802"|"200830:1241856"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200830:1568260"|"200830:1243982"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"200830:1568260"|"200830:1243983"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"200830:1568267"|"200830:1243999"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"200830:1568267"|"200830:1244000"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Shaffton component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of loamy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.    This soil does not meet hydric criteria."|"200830:265147"|"200830:1241855"
|"SOI5 description"|||"THE SHAFFTON SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOAMY ALLUVIUM ON FLOOD PLAINS AND LOW STREAM TERRACES. THE SURFACE SOIL IS A BLACK AND VERY DARK GRAYISH BROWN LOAM 13 INCHES THICK. THE SUBSOIL IS BROWN, DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED LOAM IN UPPER 23 INCHES AND GRAYISH BROWN LOAMY SAND IN LOWER 3 INCHES. THE SUBSTRATUM IS 6 INCHES OF GRAY SILTY CLAY LOAM OVER GRAYISH BROWN COARSE SAND. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND PASTURELAND."|"200830:265147"|"200830:169177"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200830:265148"|"200830:1241857"
|"SOI5 description"|||"THE EDWARDSVILLE SERIES CONSISTS OF VERY DEEP SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS UNDER PRAIRIE VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILT LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAYISH BROWN. GRAYISH BROWN, AND LIGHT BROWNISH GRAY SILTY CLAY LOAM IN UPPER 34 INCHES AND LIGHT BROWNISH GRAY SILT LOAM IN THE LOWER 8 INCHES. THE SUBSTRATUM IS LIGHT BROWNISH GRAY SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES IN THE SUBSOIL AND IN THE SUBSTRATUM. MOST AREAS ARE CROPPED."|"200831:265149"|"200831:169178"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Edwardsville component makes up 40 percent of the map unit. Slopes are 1 to 4 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 5 percent.    This soil does not meet hydric criteria."|"200831:265149"|"200831:1241870"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200831:265150"|"200831:1241872"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents component makes up 30 percent of the map unit. Slopes are 1 to 4 percent.   Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches.     This soil does not meet hydric criteria."|"200831:290106"|"200831:1241871"
|"SOI5 description"|||"THE WINFIELD SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOIL FORMED IN LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER AND SUBSURFACE LAYER ARE BROWN SILT LOAM 10 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 4 INCHES, YELLOWISH BROWN SILTY CLAY LOAM IN NEXT 16 INCHES AND LIGHT BROWNISH GRAY, BROWN, YELLOWISH BROWN AND GRAY MOTTLED SILTY CLAY LOAM IN LOWER 24 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES RANGE FROM 2 TO 35 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200832:265151"|"200832:169179"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Winfield component makes up 40 percent of the map unit. Slopes are 2 to 8 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is moderately well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 33 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.    This soil does not meet hydric criteria."|"200832:265151"|"200832:1241873"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200832:265152"|"200832:1241875"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents component makes up 30 percent of the map unit. Slopes are 2 to 8 percent.   Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches.     This soil does not meet hydric criteria."|"200832:290107"|"200832:1241874"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"200833:1164095"|"200833:1241850"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200833:1164095"|"200833:821157"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200833:1568284"|"200833:1244352"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Piasa soil is a minor component."|"200833:1568284"|"200833:1244353"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200833:276476"|"200833:1241849"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oconee component makes up 40 percent of the map unit. Slopes are 2 to 5 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.    This soil does not meet hydric criteria."|"200833:276477"|"200833:1241847"
|"SOI5 description"|||"THE OCONEE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM AND SILTY CLAY 42 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 7 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200833:276477"|"200833:183075"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Orthents component makes up 30 percent of the map unit. Slopes are 2 to 5 percent.   Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches.     This soil does not meet hydric criteria."|"200833:290100"|"200833:1241848"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"200834:1568266"|"200834:1243997"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"200834:1568266"|"200834:1243996"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"200834:1568274"|"200834:1244333"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"200834:1568274"|"200834:1244332"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200834:276480"|"200834:1241867"
|"SOI5 description"|||"THE LANDES SERIES, WELL DRAINED, CONSISTS OF WELL DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN FINE SANDY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK BROWN AND BROWN LOAM IN UPPER 9 INCHES, BROWN AND DARK YELLOWISH BROWN FINE SANDY LOAM IN NEXT 9 INCHES AND DARK YELLOWISH BROWN AND BROWN LOAMY SAND IN LOWER 4 INCHES. THE SUBSTRATUM IS YELLOWISH BROWN SAND WITH FEW FINE GRAVEL. SLOPES RANGE FROM 0 TO 7 PERCENT. CROPLAND IS THE MAIN USE."|"200834:276483"|"200834:183703"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Landes component makes up 40 percent of the map unit. Slopes are 2 to 5 percent. This component is on flood plains. The parent material consists of sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is high.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.    This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 10 percent."|"200834:276483"|"200834:1241865"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fluvents component makes up 30 percent of the map unit. Slopes are 2 to 5 percent.  The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during March, April, May, June.     This soil does not meet hydric criteria."|"200834:290077"|"200834:1241866"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is occasionally flooded. It is occasionally ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, November, December. Organic matter content in the surface horizon is about 4 percent.    This soil meets hydric criteria."|"200835:1568272"|"200835:1244329"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"200835:1568272"|"200835:1244328"
|"SOI5 description"|||"THE BEAUCOUP SERIES CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY LOAM 15 INCHES THICK. THE SUBSOIL IS DARK GRAY AND GRAY SILTY CLAY LOAM IN UPPER 33 INCHES AND GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM IN LOWER 12 INCHES. THE SUBSTRATUM IS DARK GRAY STRATIFIED SILT LOAM AND SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"200835:1568273"|"200835:1244330"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Beaucoup component makes up 90 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 6 percent.  Nonirrigated land capability classification is 2w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"200835:1568273"|"200835:1244331"
|"SOI5 description"|||"THE TICE SERIES, RARELY FLOODED, CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN SILTY CLAY LOAM 13 INCHES THICK. THE SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY LOAM IN UPPER 7 INCHES, DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SILTY CLAY LOAM IN NEXT 21 INCHES AND GRAYISH BROWN MOTTLED STRATIFIED LOAM AND SILTY CLAY LOAM IN LOWER 9 INCHES. THE SUBSTRATUM IS GRAY MOTTLED STRATIFIED SILTY CLAY LOAM AND LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. CROPLAND IS MAIN USE."|"200835:276469"|"200835:182803"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Tice component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 3 percent.    This soil does not meet hydric criteria."|"200835:276469"|"200835:1241860"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200835:276470"|"200835:1241862"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fluvents component makes up 30 percent of the map unit. Slopes are 0 to 2 percent.  The parent material consists of alluvium. Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during March, April, May, June.     This soil does not meet hydric criteria."|"200835:290076"|"200835:1241861"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"200843:1568265"|"200843:1243994"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"200843:1568265"|"200843:1243995"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"200843:1568277"|"200843:1244338"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is occasionally flooded. It is occasionally ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, November, December. Organic matter content in the surface horizon is about 4 percent.    This soil meets hydric criteria."|"200843:1568277"|"200843:1244339"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200843:276486"|"200843:1241878"
|"SOI5 description"|||"THE NAMEOKI SERIES, DRAINED, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN AND BROWN SILTY CLAY IN UPPER 16 INCHES AND DARK GRAYISH BROWN STRATIFIED CLAY LOAM, SILTY CLAY LOAM, SILT LOAM, AND LOAM IN LOWER 26 INCHES. THE SUBSTRATUM IS GRAYISH BROWN STRATIFIED SILT LOAM AND VERY FINE SANDY LOAM. REDOXIMORPHIC FEATURES ARE BELOW A DEPTH OF 12 INCHES. CROPLAND"|"200843:276490"|"200843:183704"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Nameoki component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.    This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"200843:276490"|"200843:1241876"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fluvents component makes up 30 percent of the map unit. Slopes are 0 to 2 percent.  The parent material consists of cut and fill. Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is occasionally flooded. It is not ponded. A seasonal zone of water saturation is at 27 inches during March, April, May, June.     This soil does not meet hydric criteria."|"200843:290078"|"200843:1241877"
|"SOI5 description"|||"THE AMBRAW SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN ALLUVIUM ON FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN AND VERY DARK GRAY CLAY LOAM 14 INCHES THICK. THE SUBSOIL IS DARK GRAY MOTTLED CLAY LOAM IN UPPER 23 INCHES AND DARK GRAY MOTTLED SANDY CLAY LOAM WITH LOAM AND SANDY LOAM STRATA IN LOWER 8 INCHES. THE SUBSTRATUM IS DARK GRAY MOTTLED SANDY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"200844:1568259"|"200844:1243980"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Ambraw soil is a minor component."|"200844:1568259"|"200844:1243981"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oakville component makes up 40 percent of the map unit. Slopes are 2 to 5 percent. This component is on terraces. The parent material consists of sandy eolian deposits. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is high. Available water to a depth of 60 inches is low.  Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.    This soil does not meet hydric criteria."|"200844:275408"|"200844:1241881"
|"SOI5 description"|||"THE OAKVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN FINE SAND SEDIMENTS ON OUTWASH AND LAKE PLAINS, MORAINES, AND BEACH RIDGES. THE SURFACE LAYER IS VERY DARK GRAYISH BROWN FINE SAND 7 INCHES THICK. THE SUBSOIL IS STRONG BROWN, YELLOWISH BROWN AND BROWN FINE SAND 27 INCHES THICK. THE SUBSTRATUM IS PALE BROWN FINE SAND. SLOPES RANGE FROM 0 TO 60 PERCENT. MOST AREAS ARE IN WOODLAND OR IDLE CROPLAND."|"200844:275408"|"200844:183588"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Urban land is a miscellaneous area."|"200844:276491"|"200844:1241883"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Psamments component makes up 30 percent of the map unit. Slopes are 2 to 5 percent.   Depth to a root restrictive layer is greater than 60 inches.   Available water to a depth of 60 inches is very low. Shrink-swell potential is low. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches.     This soil does not meet hydric criteria."|"200844:290079"|"200844:1241882"
|"SOI5 description"|||"THE RUMA SERIES CONSISTS OF VERY DEEP WELL DRAINED SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING SILTY PEDISEDIMENT UNDER FOREST VEGETATION ON TILL PLAINS. THE SURFACE SOIL IS MIXED DARK YELLOWISH BROWN AND YELLOWISH BROWN SILTY CLAY LOAM 5 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN UPPER 35 INCHES AND YELLOWISH BROWN SILT LOAM IN LOWER 8 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. MOST AREAS ARE CROPPED."|"202261:277551"|"202261:185566"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Ruma component makes up 50 percent of the map unit. Slopes are 18 to 35 percent. This component is on ground moraines. The parent material consists of LOESS OVER SILTY PEDISEDIMENT. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 60 inches during February, March, April. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"202261:277551"|"202261:1241824"
|"SOI5 description"|||"THE HICKORY SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN GLACIAL TILL THAT CAN BE CAPPED WITH A THIN LAYER OF LOESS ON TILL PLAINS.THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK.THE SUBSURFACE LAYER IS LIGHT YELLOWISH BROWN SILT LOAM 8 INCHES THICK.THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN CLAY LOAM IN UPPER 34 INCHES AND LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAM IN LOWER 19 INCHES.THE SUBSTRATUM IS YELLOWISH BROWN, STRONG BROWN AND LIGHT GRAY LOAM."|"202261:277552"|"202261:185567"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hickory component makes up 40 percent of the map unit. Slopes are 18 to 35 percent.  The parent material consists of TILL. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"202261:277552"|"202261:1241825"
|"SOI5 description"|||"THE AQUENTS CONSISTS OF DEEP SOILS THAT ARE SATURATED AND PONDED DURING PORTIONS OF THE GROWING SEASON IN MOST YEARS. THEY ARE MOSTLY GRAYISH IN THE UPPER 40 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT."|"202263:277553"|"202263:185568"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fluvaquents, clayey component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is high. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, June, November, December. Organic matter content in the surface horizon is about 2 percent.    This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent."|"202263:277553"|"202263:1241943"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Pierron component makes up 50 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of LOESS. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"202268:277560"|"202268:1241826"
|"SOI5 description"|||"THE PIERRON SERIES CONSISTS OF VERY DEEP POORLY DRAINED, VERY SLOWLY PERMEABLE SOILS FORMED IN LOESS, OR IN LOESS AND THE UNDERLYING DRIFT ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 8 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM 12 INCHES THICK. THE SUBSOIL IS LIGHT BROWNISH GRAY AND LIGHT OLIVE GRAY SILTY CLAY AND SILTY CLAY LOAM 46 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN SILT LOAM. THE SOIL CONTAINS REDOXIMORPHIC FEATURES THROUGHOUT. SLOPE RANGES FROM 0 TO 2 PERCENT. MOST AREAS ARE CROPPED."|"202268:277560"|"202268:185571"
|"SOI5 description"|||"THE COULTERVILLE VARIANT CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS AND THE UNDERLING SEDIMENTS ON TILL PLAINS. THE SURFACE SOIL IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE SOIL IS GRAYISH BROWN SILT LOAM 3 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY, MOTTLED SILTY CLAY LOAM IN THE UPPER 27 INCHES AND GRAY MOTTLED SILT LOAM IN THE LOWER 21 INCHES. SLOPES RANGE FROM 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"202268:277561"|"202268:185572"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Burksville component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is moderate. This soil is not flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 5 percent. The soil has a very slightly saline horizon within 30 inches of the soil surface. The soil has a slightly sodic horizon within 30 inches of the soil surface."|"202268:277561"|"202268:1241827"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 50 percent of the map unit. Slopes are 18 to 35 percent. This component is on ground moraines. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"202273:277567"|"202273:1181258"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"202273:277567"|"202273:185573"
|"SOI5 description"|||"THE HICKORY SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS FORMED IN GLACIAL TILL THAT CAN BE CAPPED WITH A THIN LAYER OF LOESS ON TILL PLAINS.THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 4 INCHES THICK.THE SUBSURFACE LAYER IS LIGHT YELLOWISH BROWN SILT LOAM 8 INCHES THICK.THE SUBSOIL IS YELLOWISH BROWN AND DARK YELLOWISH BROWN CLAY LOAM IN UPPER 34 INCHES AND LIGHT YELLOWISH BROWN AND YELLOWISH BROWN LOAM IN LOWER 19 INCHES.THE SUBSTRATUM IS YELLOWISH BROWN, STRONG BROWN AND LIGHT GRAY LOAM."|"202273:277572"|"202273:185574"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Hickory component makes up 40 percent of the map unit. Slopes are 18 to 35 percent. This component is on ground moraines. The parent material consists of till. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 6e.  This soil does not meet hydric criteria."|"202273:277572"|"202273:1181259"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Fults component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is occasionally flooded. It is frequently ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil meets hydric criteria."|"202275:1568264"|"202275:1243992"
|"SOI5 description"|||"THE FULTS SERIES, DRAINED, CONSISTS OF VERY DEEP, POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON GENTLY UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAY SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS DARK GRAY CLAY IN UPPER 20 INCHES AND DARK GRAY CLAY LOAM AND SANDY CLAY LOAM IN LOWER 10 INCHES. IS THE MAIN USE."|"202275:1568264"|"202275:1243991"
|"SOI5 description"|||"THE DARWIN SERIES, COMMONLY FLOODED CONSISTS OF POORLY AND VERY POORLY DRAINED SOILS FORMED IN CLAYEY ALLUVIUM ON FLOODPLAINS. THE SURFACE LAYER IS VERY DARK GRAY SILTY CLAY 14 INCHES THICK. THE SUBSOIL IS DARK GRAY AND DARK SILTY CLAY IN UPPER 32 INCHES AND GRAY SILTY CLAY LOAM IN LOWER 10 INCHES. THE SUBSTRATUM IS GRAY SILTY CLAY LOAM. SLOPES ARE 0 TO 2 PERCENT. AREAS ARE USED FOR CROPLAND AND WOODLAND."|"202275:1568283"|"202275:1244350"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Darwin component makes up 40 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is moderate.  Shrink-swell potential is very high. This soil is occasionally flooded. It is occasionally ponded. A seasonal zone of water saturation is at 6 inches during January, February, March, April, May, November, December. Organic matter content in the surface horizon is about 4 percent.    This soil meets hydric criteria."|"202275:1568283"|"202275:1244351"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Nameoki component makes up 85 percent of the map unit. Slopes are 0 to 2 percent. This component is on flood plains. The parent material consists of clayey alluvium over loamy and sandy alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is frequently flooded. It is not ponded. A seasonal zone of water saturation is at 18 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 4 percent.  Nonirrigated land capability classification is 3w.  This soil does not meet hydric criteria. The calcium carbonate equivalent within 40 inches, typically, does not exceed 3 percent."|"202275:289051"|"202275:1241889"
|"SOI5 description"|||"THE NAMEOKI SERIES, DRAINED, CONSISTS OF VERY DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SLACKWATER SEDIMENTS AND THE UNDERLYING STRATIFIED LOAMY AND SANDY ALLUVIUM ON UNDULATING FLOOD PLAINS. THE SURFACE SOIL IS VERY DARK GRAYISH BROWN SILTY CLAY 12 INCHES THICK. THE SUBSOIL IS VERY DARK GRAYISH BROWN AND BROWN SILTY CLAY IN UPPER 16 INCHES AND DARK GRAYISH BROWN STRATIFIED CLAY LOAM, SILTY CLAY LOAM, SILT LOAM, AND LOAM IN LOWER 26 INCHES. THE SUBSTRATUM IS GRAYISH BROWN STRATIFIED SILT LOAM AND VERY FINE SANDY LOAM. REDOXIMORPHIC FEATURES ARE BELOW A DEPTH OF 12 INCHES. CROPLAND"|"202275:289051"|"202275:185631"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"207591:265126"|"207591:169159"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 85 percent of the map unit. Slopes are 5 to 10 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 4e.  This soil does not meet hydric criteria."|"207591:265126"|"207591:1241789"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"207592:265130"|"207592:169163"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 85 percent of the map unit. Slopes are 18 to 35 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 1 percent.  Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria."|"207592:265130"|"207592:1241792"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Menfro component makes up 90 percent of the map unit. Slopes are 35 to 60 percent. This component is on loess hills. The parent material consists of loess. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is moderate. This soil is not flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 7e.  This soil does not meet hydric criteria."|"207593:265131"|"207593:1241793"
|"SOI5 description"|||"THE MENFRO SERIES CONSISTS OF DEEP, WELL DRAINED SOILS FORMED IN SILTY LOESS ON RIDGETOPS AND SIDE SLOPES. THE SURFACE LAYER IS DARK BROWN SILT LOAM 6 INCHES THICK. THE SUBSURFACE LAYER IS BROWN SILT LOAM 6 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM IN UPPER 3 INCHES AND BROWN, DARK BROWN AND DARK YELLOWISH BROWN SILTY CLAY LOAM IN LOWER 53 INCHES. THE SUBSTRATUM IS BROWN SILT LOAM. SLOPES RANGE FROM 2 TO 60 PERCENT. CLEARED AREAS ARE USED FOR CROPLAND, HAYLAND OR PASTURE; STEEPER AREAS ARE USED FOR WOODLAND."|"207593:265131"|"207593:169164"
|"SOI5 description"|||"THE COWDEN SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY AND GRAY SILT LOAM 11 INCHES THICK. THE SUBSOIL IS GRAYISH BROWN AND LIGHT BROWNISH GRAY SILTY CLAY LOAM 31 INCHES THICK. THE SUBSTRATUM IS GRAY SILT LOAM. SLOPES RANGE FROM 0 TO 4 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"207594:1567519"|"207594:1239806"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Cowden soil is a minor component."|"207594:1567519"|"207594:1239807"
|"SOI5 description"|||"THE PIASA SERIES CONSISTS OF POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAY SILT LOAM 4 INCHES THICK. THE MOTTLED SUBSOIL IS DARK GRAYISH BROWN SILTY CLAY AND SILTY CLAY LOAM IN UPPER 25 INCHES AND DARK GRAYISH BROWN AND GRAYISH BROWN SILTY CLAY LOAM AND SILT LOAM IN LOWER 11 INCHES. THE SUBSTRATUM IS GRAY MOTTLED SILT LOAM. SLOPES ARE 0 TO 2 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"207594:1567520"|"207594:1239809"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Piasa soil is a minor component."|"207594:1567520"|"207594:1239808"
|"SOI5 description"|||"THE OCONEE SERIES CONSISTS OF SOMEWHAT POORLY DRAINED SOILS FORMED IN LOESS ON UPLANDS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 8 INCHES THICK. THE SUBSURFACE LAYER IS DARK GRAYISH BROWN AND GRAYISH BROWN MOTTLED SILT LOAM 8 INCHES THICK. THE SUBSOIL IS BROWN, GRAYISH BROWN AND LIGHT BROWNISH GRAY MOTTLED SILTY CLAY LOAM AND SILTY CLAY 42 INCHES THICK. THE SUBSTRATUM IS BROWN MOTTLED SILT LOAM. SLOPES RANGE FROM 0 TO 7 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"207594:265137"|"207594:169170"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Oconee component makes up 94 percent of the map unit. Slopes are 0 to 2 percent. This component is on ground moraines. The parent material consists of loess over silty pedisediment. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is somewhat poorly drained.  Water movement in the most restrictive layer is moderately low.  Available water to a depth of 60 inches is high.  Shrink-swell potential is high. This soil is not flooded. It is not ponded. A seasonal zone of water saturation is at 15 inches during January, February, March, April, May. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2w.  This soil does not meet hydric criteria."|"207594:265137"|"207594:1181193"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major soil components.  The Miscellaneous water is a miscellaneous area."|"207595:284906"|"207595:1218150"
|"SOI5 description"|||"THE TWOMILE SERIES CONSISTS OF DEEP, POORLY DRAINED SOILS FORMED IN LOESS OR SILTY ALLUVIUM ON STREAM TERRACES. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SILT LOAM SUBSURFACE LAYER IS GRAYISH BROWN AND LIGHT BROWNISH GRAY IN UPPER 15 INCHES AND GRAY AND COMPACT AND BRITTLE WITH MANY CONCRETIONS IN LOWER 9 INCHES. THE SUBSOIL IS GRAYISH BROWN AND GRAY SILTY CLAY LOAM 29 INCHES THICK. THE SUBSTRATUM IS GRAYISH BROWN AND GRAY CLAY LOAM. SLOPES ARE 0 TO 3 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURE AND HAYLAND."|"208932:1468530"|"208932:1074164"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Twomile soil is a minor component."|"208932:1468530"|"208932:1181330"
05/25/2006|"Nontechnical description"|"GENSOIL"||"The Drury component makes up 97 percent of the map unit. Slopes are 2 to 5 percent. This component is on alluvial fans. The parent material consists of local silty alluvium. Depth to a root restrictive layer is greater than 60 inches. The natural drainage class is well drained.  Water movement in the most restrictive layer is moderately high.  Available water to a depth of 60 inches is very high.  Shrink-swell potential is low. This soil is rarely flooded. It is not ponded. There is no zone of water saturation within a depth of 72 inches. Organic matter content in the surface horizon is about 2 percent.  Nonirrigated land capability classification is 2e.  This soil does not meet hydric criteria."|"208932:290167"|"208932:186524"
|"SOI5 description"|||"THE DRURY SERIES CONSISTS OF WELL DRAINED SOILS FORMED IN SILTY ALLUVIUM ON STREAM TERRACES AND FOOTSLOPES. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 7 INCHES THICK. THE SUBSURFACE LAYER IS MIXED BROWN AND YELLOWISH BROWN SILT LOAM 5 INCHES THICK. THE SUBSOIL IS DARK YELLOWISH BROWN SILT LOAM 23 INCHES THICK. THE SUBSTRATUM IS DARK YELLOWISH BROWN SILT LOAM. SLOPES RANGE FROM 0 TO 30 PERCENT. AREAS ARE USED FOR CROPLAND, PASTURELAND AND WOODLAND."|"208932:290167"|"208932:1181329"
05/25/2006|"Nontechnical description"|"GENSOIL"||"Generated brief soil descriptions are created for major components.  The Vesser soil is a minor component."|"208932:910025"|"208932:564833"
|"SOI5 description"|||"THE VESSER SERIES CONSISTS OF SOMEWHAT POORLY OR POORLY DRAINED SOILS FORMED IN SILTY ALLUVIUM UNDER GRASSES ON HIGH BOTTOM LANDS, FOOTSLOPES AND FANS. THE SURFACE LAYER IS VERY DARK GRAY SILT LOAM 12 INCHES THICK. THE SUBSURFACE LAYER IS VERY DARK GRAY AND DARK GRAY SILT LOAM 19 INCHES THICK. THE SUBSOIL IS DARK GRAY AND VERY DARK GRAY SILTY CLAY LOAM. SLOPES RANGE FROM 0 TO 5 PERCENT. MOST AREAS ARE USED FOR CROPLAND."|"208932:910025"|"208932:1181331"
