|"Nontechnical description"|"SO5"|"PA0036"|"THE ALBRIGHTS SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND FINE GRAINED SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH GRAY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL LAYERS FROM 8 TO 30 INCHES ARE REDDISH BROWN SILT LOAM AND YELLOWISH RED SILT LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 30 TO 55 INCHES IS REDDISH BROWN AND STRONG BROWN CHANNERY SILT LOAM AND CHANNERY SILTY CLAY LOAM."|"541947"|"541947:m:458477"
|"Nontechnical description"|"AGR"|"0611"|"Albrights soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is 20 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is low. The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"541947"|"541947:m:458478"
|"Nontechnical description"|"SO5"|"PA0036"|"THE ALBRIGHTS SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND FINE GRAINED SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH GRAY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL LAYERS FROM 8 TO 30 INCHES ARE REDDISH BROWN SILT LOAM AND YELLOWISH RED SILT LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 30 TO 55 INCHES IS REDDISH BROWN AND STRONG BROWN CHANNERY SILT LOAM AND CHANNERY SILTY CLAY LOAM."|"541948"|"541948:m:458479"
|"Nontechnical description"|"AGR"|"0612"|"Albrights soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 20 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 3e."|"541948"|"541948:m:458480"
|"Nontechnical description"|"SO5"|"PA0037"|"THE ALBRIGHTS SERIES CONSISTS OF VERY DEEP, MODERATELY WELL AND SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND FINE GRAINED SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH GRAY VERY STONY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL LAYERS FROM 8 TO 21 INCHES ARE REDDISH BROWN SILT LOAM AND CHANNERY CLAY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 21 TO 48 INCHES IS REDDISH BROWN AND WEAK RED CHANNERY LOAM. THE SUBSTRATUM FROM 48 TO 60 INCHES IS WEAK RED CHANNERY LOAM."|"541949"|"541949:m:458481"
|"Nontechnical description"|"AGR"|"0613"|"Albrights soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is 20 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 6s."|"541949"|"541949:m:458482"
|"Nontechnical description"|"SO5"|"PA0037"|"THE ALBRIGHTS SERIES CONSISTS OF VERY DEEP, MODERATELY WELL AND SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND FINE GRAINED SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH GRAY VERY STONY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL LAYERS FROM 8 TO 21 INCHES ARE REDDISH BROWN SILT LOAM AND CHANNERY CLAY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 21 TO 48 INCHES IS REDDISH BROWN AND WEAK RED CHANNERY LOAM. THE SUBSTRATUM FROM 48 TO 60 INCHES IS WEAK RED CHANNERY LOAM."|"541950"|"541950:m:458483"
|"Nontechnical description"|"AGR"|"0614"|"Andover soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a mountain slope.  The runoff class is very high.  The depth to a restrictive feature is 16 to 26 inches to fragipan. It is poorly drained.  The slowest permeability within 60 inches is slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 7s."|"541950"|"541950:m:458484"
|"Nontechnical description"|"SO5"|"PA0093"|"THE ANDOVER SERIES CONSISTS OF VERY DEEP, POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN LOAMY COLLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN COBBLY LOAM SURFACE LAYER 7 INCHES THICK. THE MOTTLED SUBSOIL FROM 7 TO 18 INCHES IS LIGHT BROWNISH GRAY COBBLY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 18 TO 48 INCHES IS MOTTLED YELLOWISH BROWN AND BROWN COBBLY CLAY LOAM. THE SUBSTRATUM FROM 48 TO 60 INCHES IS BROWN GRAVELLY SANDY CLAY LOAM."|"541951"|"541951:m:458485"
|"Nontechnical description"|"AGR"|"0615"|"Andover soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a mountain slope.  The runoff class is very high.  The depth to a restrictive feature is 16 to 26 inches to fragipan. It is poorly drained.  The slowest permeability within 60 inches is slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 4w."|"541951"|"541951:m:458486"
|"Nontechnical description"|"SOI"|"130"|"The Klinesville series consists of shallow, well drained soils on uplands. They formed in material weathered from shale, siltstone, and sandstone. Typically these soils have a dark reddish brown very shaly silt loam surface layer 5 inches thick. The subsoil from 5 to 15 inches is reddish brown very shaly silt loam. The substratum from 15 to 19 inches is weak red weathered shale fragments. Bedrock is at 19 inches."|"927059"|"927059:m:1665585"
|"Nontechnical description"|"AGR"|"00977"|"Soil KLINESVILLE is 10 - 20 inches to bedrock. Permeability is MODERATELY RAPID and available water holding capacity is VERY LOW. A water table when present is >6 - feet. The soil productivity is NOT SUITED TO CROPLAND and the capability subclass is 7E."|"927059"|"927059:m:1665582"
|"Nontechnical description"|"AGR"|"00978"|"Soil ROCK OUTCROP is 0 - inches to bedrock. Permeability is VERY SLOW and available water holding capacity is VERY LOW. A water table when present is >6 - feet. The soil productivity is NOT SUITED TO CROPLAND and the capability subclass is 8S."|"927059"|"927059:m:1665583"
|"Nontechnical description"|"ENG"|"009KoF"|"Shallow, excessively drained Klinesville soils and bedrock outcrops on very steep slopes make up these delineations. Depth to bedrock, very steep slopes, rock outcrops are the main limitations for most all uses."|"927059"|"927059:m:1665584"
03/26/2002|"Nontechnical description"|"AGR"|||"927072"|"927072:m:1665586"
03/26/2002|"Nontechnical description"|"AGR"||"Dekalb soils make up 60 percent of the map unit. This soil is well drained.  The depth to a restrictive feature is 20 to 40 inches to bedrock (lithic).  The slowest soil permeability within a depth of 60 inches is moderately rapid.  Available water capacity to a depth of 60 inches is very low, and shrink swell potential is low. Annual flooding is none, and annual ponding is none.  The minimum depth to a water table is greater than 6 feet.  It is nonirrigated land capability subclass 7s.  This soil is not suitable for cultivated crops.  This component is not a hydric soil.  The assigned Kw erodibility factor is .17.

Hazleton soils make up 25 percent of the map unit. This soil is well drained.  The depth to a restrictive feature is 40 inches bedrock (lithic).  The slowest soil permeability within a depth of 60 inches is moderately rapid.  Available water capacity to a depth of 60 inches is low, and shrink swell potential is low. Annual flooding is none, and annual ponding is none.  The minimum depth to a water table is greater than 6 feet.  It is nonirrigated land capability subclass 7s.  This soil is not suitable for cultivated crops.  This component is not a hydric soil.  The assigned Kw erodibility factor is .15."|"927073"|"927073:m:1665587"
|"Nontechnical description"|"AGR"|"0616"|"Soil ANDOVER is >60 - 96 inches to bedrock. Permeability is SLOW and available water holding capacity is LOW. A water table when present is 0 - 0.5 feet. The soil productivity is NOT SUITED TO CROPLAND and the capability subclass is 7S."|"541952"|"541952:m:458488"
|"Nontechnical description"|"SO5"|"PA0092"|"THE ANDOVER SERIES CONSISTS OF DEEP, POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN LOAM SURFACE LAYER 7 INCHES THICK. THE MOTTLED SUBSOIL FROM 7 TO 18 INCHES IS LIGHT BROWNISH GRAY COBBLY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 18 TO 48 INCHES IS MOTTLED YELLOWISH BROWN AND BROWN COBBLY CLAY LOAM. THE SUBSTRATUM FROM 48 TO 60 INCHES IS BROWN GRAVELLY SANDY CLAY LOAM."|"541952"|"541952:m:458487"
|"Nontechnical description"|"SO5"|"WV0008"|"THE ATKINS SERIES CONSISTS OF DEEP, POORLY DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN ALLUVIAL MATERIAL. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A DARK GRAY SILT LOAM SURFACE LAYER 2 INCHES THICK UNDERLAIN BY 8 INCHES OF GRAY SILT LOAM. THE SUBSOIL FROM 10 TO 20 INCHES IS GRAY HEAVY SILT LOAM MOTTLED WITH STRONG BROWN. FROM 20 T0 34 INCHES, THE SUBSOIL IS MIXED GRAY AND STRONG BROWN SILTY CLAY LOAM. THE SUBSTRATUM FROM 34 TO 60 INCHES IS MIXED GRAY AND STRONG BROWN SILT LOAM."|"541953"|"541953:m:458489"
|"Nontechnical description"|"AGR"|"0617"|"Atkins soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a drainageway.  The runoff class is very high.  It is poorly drained.  The slowest permeability within 60 inches is slow.  Available water capacity is high and shrink swell potential is low. This soil is subject to frequent flooding and is not ponded.  The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 4w."|"541953"|"541953:m:458490"
|"Nontechnical description"|"AGR"|"0618"|"Berks soils make up 50 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7e.

 Weikert soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7e."|"541954"|"541954:m:458491"
|"Nontechnical description"|"SO5"|"PA0004"|"THE BERKS SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN CHANNERY LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL IS FRIABLE AND ABOUT 16 INCHES THICK. IN A SEQUENCE FROM THE TOP, THE UPPER 7 INCHES IS YELLOWISH BROWN CHANNERY LOAM; THE NEXT 4 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM; AND THE LOWER 5 INCHES IS STRONG BROWN VERY CHANNERY LOAM. THE FRIABLE SUBSTRATUM IS YELLOWISH-BROWN VERY CHANNERY LOAM OVERLYING FRACTURED BEDROCK AT A DEPTH OF 33 IN."|"541954"|"541954:m:458493"
|"Nontechnical description"|"SO5"|"PA0024"|"THE WEIKERT SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN CHANNERY SILT LOAM SURFACE LAYER 7 INCHES THICK. THE SUBSOIL FROM 7 TO 14 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 7 TO 18 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. BEDROCK IS AT 18 INCHES."|"541954"|"541954:m:458494"
|"Nontechnical description"|"SO5"|"NY0189"|"THE BARBOUR SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON FLOODPLAINS, ALLUVIAL FANS, AND LOW TERRACES. THEY FORMED IN ALLUVIAL DEPOSITS DERIVED FROM REDDISH SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH BROWN LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL LAYERS FROM 6 TO 26 INCHES ARE FRIABLE REDDISH BROWN SILT LOAM AND GRAVELLY LOAM. THE SUBSTRATUM FROM 26 TO 60 INCHES IS REDDISH-BROWN VERY GRAVELLY LOAMY SAND."|"541955"|"541955:m:458495"
|"Nontechnical description"|"AGR"|"06110"|"Barbour soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low. This soil is subject to occasional flooding and is not ponded.  The top of the seasonal high water table ranges from 36 to 72 inches.  Major component is not a hydric soil.  Land capability class 1."|"541955"|"541955:m:458496"
|"Nontechnical description"|"SO5"|"NY0189"|"THE BARBOUR SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON FLOODPLAINS, ALLUVIAL FANS, AND LOW TERRACES. THEY FORMED IN ALLUVIAL DEPOSITS DERIVED FROM REDDISH SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY, THESE SOILS HAVE A DARK REDDISH BROWN LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL LAYERS FROM 6 TO 26 INCHES ARE FRIABLE REDDISH BROWN SILT LOAM AND GRAVELLY LOAM. THE SUBSTRATUM FROM 26 TO 60 INCHES IS REDDISH-BROWN VERY GRAVELLY LOAMY SAND."|"541956"|"541956:m:458497"
|"Nontechnical description"|"AGR"|"06111"|"Barbour soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low. This soil is subject to rare flooding and is not ponded.  The top of the seasonal high water table ranges from 36 to 72 inches.  Major component is not a hydric soil.  Land capability class 1."|"541956"|"541956:m:458498"
|"Nontechnical description"|"SO5"|"NY0231"|"THE BASHER SERIES CONSIST OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN ALLUVIAL DEPOSITS DERIVED FROM REDDISH SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK REDDISH BROWN SURFACE LAYER 9 INCHES THICK. THE SUBSOIL LAYERS FROM 9 TO 27 INCHES ARE DARK REDDISH BROWN AND YELLOWISH BROWN SILT LOAM. THE SUBSTRATUM FROM 27 TO 42 INCHES IS GRAYISH BROWN AND GRAY LOAM AND FROM 42 TO 60 INCHES IT IS VERY DARK GRAY FINE SANDY LOAM. SLOPES RANGE FROM 0 TO 3 PERCENT."|"541957"|"541957:m:458499"
|"Nontechnical description"|"AGR"|"06112"|"Basher Variant soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to occasional flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2w."|"541957"|"541957:m:458500"
|"Nontechnical description"|"AGR"|"06113"|"Bedington soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541958"|"541958:m:458502"
|"Nontechnical description"|"SO5"|"PA0071"|"THE BEDINGTON SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN, CHANNERY SILT LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL FORM 10 TO 17 INCHES IS STRONG BROWN CHANNERY SILT LOAM, FROM 17 TO 35 INCHES IS YELLOW RED CHANNERY SILT LOAM AND FROM 35 TO 43 INCHES IS YELLOWISH RED VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 43 TO 63 INCHES IS . YELLOWISH RED EXTREMELY CHANNERY SILT LOAM."|"541958"|"541958:m:458501"
|"Nontechnical description"|"SO5"|"PA0071"|"THE BEDINGTON SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN, CHANNERY SILT LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL FORM 10 TO 17 INCHES IS STRONG BROWN CHANNERY SILT LOAM, FROM 17 TO 35 INCHES IS YELLOW RED CHANNERY SILT LOAM AND FROM 35 TO 43 INCHES IS YELLOWISH RED VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 43 TO 63 INCHES IS . YELLOWISH RED EXTREMELY CHANNERY SILT LOAM."|"541959"|"541959:m:458503"
|"Nontechnical description"|"AGR"|"06114"|"Bedington soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is greater than 40 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541959"|"541959:m:458504"
|"Nontechnical description"|"AGR"|"06115"|"Bedington soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541960"|"541960:m:458506"
|"Nontechnical description"|"SO5"|"PA0071"|"THE BEDINGTON SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN, CHANNERY SILT LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL FORM 10 TO 17 INCHES IS STRONG BROWN CHANNERY SILT LOAM, FROM 17 TO 35 INCHES IS YELLOW RED CHANNERY SILT LOAM AND FROM 35 TO 43 INCHES IS YELLOWISH RED VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 43 TO 63 INCHES IS . YELLOWISH RED EXTREMELY CHANNERY SILT LOAM."|"541960"|"541960:m:458505"
|"Nontechnical description"|"SO5"|"PA0004"|"THE BERKS SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN CHANNERY LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL IS FRIABLE AND ABOUT 16 INCHES THICK. IN A SEQUENCE FROM THE TOP, THE UPPER 7 INCHES IS YELLOWISH BROWN CHANNERY LOAM; THE NEXT 4 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM; AND THE LOWER 5 INCHES IS STRONG BROWN VERY CHANNERY LOAM. THE FRIABLE SUBSTRATUM IS YELLOWISH-BROWN VERY CHANNERY LOAM OVERLYING FRACTURED BEDROCK AT A DEPTH OF 33 IN."|"541961"|"541961:m:458507"
|"Nontechnical description"|"AGR"|"06116"|"Berks soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541961"|"541961:m:458508"
|"Nontechnical description"|"SO5"|"PA0004"|"THE BERKS SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN CHANNERY LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL IS FRIABLE AND ABOUT 16 INCHES THICK. IN A SEQUENCE FROM THE TOP, THE UPPER 7 INCHES IS YELLOWISH BROWN CHANNERY LOAM; THE NEXT 4 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM; AND THE LOWER 5 INCHES IS STRONG BROWN VERY CHANNERY LOAM. THE FRIABLE SUBSTRATUM IS YELLOWISH-BROWN VERY CHANNERY LOAM OVERLYING FRACTURED BEDROCK AT A DEPTH OF 33 IN."|"541962"|"541962:m:458509"
|"Nontechnical description"|"AGR"|"06117"|"Berks soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541962"|"541962:m:458510"
|"Nontechnical description"|"SO5"|"PA0004"|"THE BERKS SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN CHANNERY LOAM SURFACE LAYER 10 INCHES THICK. THE SUBSOIL IS FRIABLE AND ABOUT 16 INCHES THICK. IN A SEQUENCE FROM THE TOP, THE UPPER 7 INCHES IS YELLOWISH BROWN CHANNERY LOAM; THE NEXT 4 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM; AND THE LOWER 5 INCHES IS STRONG BROWN VERY CHANNERY LOAM. THE FRIABLE SUBSTRATUM IS YELLOWISH-BROWN VERY CHANNERY LOAM OVERLYING FRACTURED BEDROCK AT A DEPTH OF 33 IN."|"541963"|"541963:m:458511"
|"Nontechnical description"|"AGR"|"06118"|"Berks soils make up 50 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e.

 Weikert soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"541963"|"541963:m:458512"
|"Nontechnical description"|"SO5"|"PA0193"|"THE BIRDSBORO SERIES CONSISTS OF VERY DEEP, WELL TO MODERATELY WELL DRAINED SOILS ON TERRACES AND ALLUVIAL FANS. THEY FORMED IN STREAM DEPOSITS WASHED FROM UPLANDS UNDERLAIN BY RED SANDSTONE, SHALE AND SILTSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILT LOAM SURFACE LAYER ABOUT 10 INCHES THICK. THE SUBSOIL BETWEEN 10 AND 46 INCHES IS REDDISH BROWN AND BROWN SILTY CLAY LOAM, LOAM AND SANDY CLAY LOAM. THE SUBSTRATUM FROM 46 TO 70 INCHES IS REDDISH BROWN VERY GRAVELLY CLAY LOAM."|"541964"|"541964:m:458514"
|"Nontechnical description"|"AGR"|"06120"|"Birdsboro soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541964"|"541964:m:458515"
|"Nontechnical description"|"SO5"|"PA0097"|"THE BLAIRTON SERIES CONSISTS OF MODERATELY DEEP, SOMEWHAT POORLY AND MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM GRAY SHALE. TYPICALLY THESE SOILS HAVE A DARK GRAYSIH BROWN SILT LOAM SURFACE LAYER ABOUT 9 INCHES THICK. THE SUBSOIL LAYERS FROM 9 TO 34 INCHES IS YELLOWISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM, SHALY SILTY CLAY LOAM AND SHALY SILT LOAM. THE SUBSTRATUM FROM 34 TO 38 INCHES IS GRAYISH BROWN VERY SHALY LOAM."|"541965"|"541965:m:458516"
|"Nontechnical description"|"AGR"|"06121"|"Blairton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is high.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 3w."|"541965"|"541965:m:458517"
|"Nontechnical description"|"AGR"|"06122"|"Blairton soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is moderately well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 4e."|"541966"|"541966:m:458519"
|"Nontechnical description"|"SO5"|"PA0097"|"THE BLAIRTON SERIES CONSISTS OF MODERATELY DEEP, SOMEWHAT POORLY AND MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM GRAY SHALE. TYPICALLY THESE SOILS HAVE A DARK GRAYSIH BROWN SILT LOAM SURFACE LAYER ABOUT 9 INCHES THICK. THE SUBSOIL LAYERS FROM 9 TO 34 INCHES IS YELLOWISH BROWN AND LIGHT BROWNISH GRAY SILT LOAM, SHALY SILTY CLAY LOAM AND SHALY SILT LOAM. THE SUBSTRATUM FROM 34 TO 38 INCHES IS GRAYISH BROWN VERY SHALY LOAM."|"541966"|"541966:m:458518"
|"Nontechnical description"|"SO5"|"PA0090"|"THE BRINKERTON SERIES CONSISTS OF VERY DEEP, POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 21 INCHES IS GRAYISH BROWN SILTY CLAY LOAM. A FIRM AND BRITTLE FRAGIPAN IS BETWEEN 21 AND 42 INCHES. IT IS GRAYISH BROWN AND PALE BROWN SILT LOAM WITH MOTTLED COLORS. THE SUBSTRATUM FROM 42 TO 60 INCHES IS BROWN CHANNERY SILT LOAM."|"541967"|"541967:m:458520"
|"Nontechnical description"|"AGR"|"06123"|"Brinkerton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a drainageway.  The runoff class is very high.  The depth to a restrictive feature is 18 to 30 inches to fragipan. It is poorly drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 4w."|"541967"|"541967:m:458521"
|"Nontechnical description"|"AGR"|"06124"|"Brinkerton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a drainageway.  The runoff class is very high.  The depth to a restrictive feature is 18 to 30 inches to fragipan. It is poorly drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 4w."|"541968"|"541968:m:458523"
|"Nontechnical description"|"SO5"|"PA0090"|"THE BRINKERTON SERIES CONSISTS OF VERY DEEP, POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 21 INCHES IS GRAYISH BROWN SILTY CLAY LOAM. A FIRM AND BRITTLE FRAGIPAN IS BETWEEN 21 AND 42 INCHES. IT IS GRAYISH BROWN AND PALE BROWN SILT LOAM WITH MOTTLED COLORS. THE SUBSTRATUM FROM 42 TO 60 INCHES IS BROWN CHANNERY SILT LOAM."|"541968"|"541968:m:458522"
|"Nontechnical description"|"SO5"|"PA0038"|"THE BUCHANAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL TO SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED FROM SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN GRAVELLY LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 27 INCHES IS MAINLY YELLOWISH BROWN GRAVELLY LOAM. A FIRM AND BRITTLE FRAGIPAN FROM 27 TO 47 INCHES IS YELLOWISH BROWN GRAVELLY LOAM. THE SUBSTRATUM FROM 47 TO 60 INCHES IS YELLOWISH BROWN GRAVELLY LOAM."|"541969"|"541969:m:458524"
|"Nontechnical description"|"AGR"|"06125"|"Buchanan soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is high.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"541969"|"541969:m:458525"
|"Nontechnical description"|"SO5"|"PA0038"|"THE BUCHANAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL TO SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED FROM SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN GRAVELLY LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 27 INCHES IS MAINLY YELLOWISH BROWN GRAVELLY LOAM. A FIRM AND BRITTLE FRAGIPAN FROM 27 TO 47 INCHES IS YELLOWISH BROWN GRAVELLY LOAM. THE SUBSTRATUM FROM 47 TO 60 INCHES IS YELLOWISH BROWN GRAVELLY LOAM."|"541970"|"541970:m:458526"
|"Nontechnical description"|"AGR"|"06126"|"Buchanan soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is high.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 3e."|"541970"|"541970:m:458527"
|"Nontechnical description"|"SO5"|"PA0038"|"THE BUCHANAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL TO SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED FROM SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN GRAVELLY LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 27 INCHES IS MAINLY YELLOWISH BROWN GRAVELLY LOAM. A FIRM AND BRITTLE FRAGIPAN FROM 27 TO 47 INCHES IS YELLOWISH BROWN GRAVELLY LOAM. THE SUBSTRATUM FROM 47 TO 60 INCHES IS YELLOWISH BROWN GRAVELLY LOAM."|"541971"|"541971:m:458528"
|"Nontechnical description"|"AGR"|"06127"|"Buchanan soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 4e."|"541971"|"541971:m:458529"
|"Nontechnical description"|"SO5"|"PA0039"|"THE BUCHANAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL TO SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED FROM SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 27 INCHES IS MAINLY YELLOWISH BROWN GRAVELLY LOAM. A FIRM AND BRITTLE FRAGIPAN FROM 27 TO 47 INCHES IS YELLOWISH BROWN GRAVELLY LOAM. THE SUBSTRATUM FROM 47 TO 60 INCHES IS YELLOWISH BROWN GRAVELLY LOAM."|"541972"|"541972:m:458530"
|"Nontechnical description"|"AGR"|"06128"|"Buchanan soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 7s."|"541972"|"541972:m:458531"
|"Nontechnical description"|"SO5"|"PA0039"|"THE BUCHANAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL TO SOMEWHAT POORLY DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED FROM SANDSTONE, SILTSTONE, AND SHALE. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 27 INCHES IS MAINLY YELLOWISH BROWN GRAVELLY LOAM. A FIRM AND BRITTLE FRAGIPAN FROM 27 TO 47 INCHES IS YELLOWISH BROWN GRAVELLY LOAM. THE SUBSTRATUM FROM 47 TO 60 INCHES IS YELLOWISH BROWN GRAVELLY LOAM."|"541973"|"541973:m:458532"
|"Nontechnical description"|"AGR"|"06129"|"Buchanan soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 6 to 36 inches.  Major component is not a hydric soil.  Land capability class 7s."|"541973"|"541973:m:458533"
|"Nontechnical description"|"SO5"|"PA0043"|"THE CALVIN SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM REDDISH SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A REDDISH BROWN CHANNERY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 29 INCHES IS REDDISH BROWN VERY CHANNERY SILT LOAM AND VERY CHANNERY LOAM. THE SUBSTRATUM FROM 29 TO 35 INCHES IS DUSKY RED EXTREMELY CHANNERY SILT LOAM. BEDROCK IS AT 35 INCHES."|"541974"|"541974:m:458535"
|"Nontechnical description"|"AGR"|"06130"|"Calvin soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541974"|"541974:m:458534"
|"Nontechnical description"|"SO5"|"PA0043"|"THE CALVIN SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM REDDISH SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A REDDISH BROWN CHANNERY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 29 INCHES IS REDDISH BROWN VERY CHANNERY SILT LOAM AND VERY CHANNERY LOAM. THE SUBSTRATUM FROM 29 TO 35 INCHES IS DUSKY RED EXTREMELY CHANNERY SILT LOAM. BEDROCK IS AT 35 INCHES."|"541975"|"541975:m:458536"
|"Nontechnical description"|"AGR"|"06131"|"Calvin soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541975"|"541975:m:458537"
|"Nontechnical description"|"AGR"|"06132"|"Calvin soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 20 to 40 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541976"|"541976:m:458539"
|"Nontechnical description"|"SO5"|"PA0043"|"THE CALVIN SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM REDDISH SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY, THESE SOILS HAVE A REDDISH BROWN CHANNERY SILT LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 29 INCHES IS REDDISH BROWN VERY CHANNERY SILT LOAM AND VERY CHANNERY LOAM. THE SUBSTRATUM FROM 29 TO 35 INCHES IS DUSKY RED EXTREMELY CHANNERY SILT LOAM. BEDROCK IS AT 35 INCHES."|"541976"|"541976:m:458538"
|"Nontechnical description"|"SO5"|"PA0033"|"THE CLARKSBURG SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN CALCAREOUS COLLUVIUM OR GLACIAL TILL, OR RESIDUUM. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 9 INCHES THICK. THE SUBSOIL IS YELLOWISH BROWN. IT IS SILT LOAM FROM 9 TO 12 INCHES, AND SILTY CLAY LOAM FROM 12 TO 48 INCHES. FROM 28 TO 48 INCHES IT IS FIRM, MOTTLED YELLOWISH BROWN SILTY CLAY LOAM. THE SUBSTRATUM, FROM 48 TO 65 INCHES IS MOTTLED STRONG BROWN GRAVELLY SILTY CLAY LOAM."|"541977"|"541977:m:458540"
|"Nontechnical description"|"AGR"|"06133"|"Clarksburg soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is 26 to 35 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"541977"|"541977:m:458541"
|"Nontechnical description"|"SO5"|"PA0058"|"THE CLYMER SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A VERY DARK GRAYISH BROWN CHANNERY LOAM SURFACE LAYER ABOUT 8 INCHES THICK. THE SUBSOIL BETWEEN 8 AND 36 INCHES IS YELLOWISH BROWN AND STRONG BROWN CHANNERY LOAM. THE SUBSTRATUM FROM 36 TO 50 INCHES IS YELLOWISH BROWN VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT ABOUT 50 INCHES."|"541978"|"541978:m:458542"
|"Nontechnical description"|"AGR"|"06134"|"Clymer soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541978"|"541978:m:458543"
|"Nontechnical description"|"SO5"|"PA0024"|"THE WEIKERT SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN CHANNERY SILT LOAM SURFACE LAYER 7 INCHES THICK. THE SUBSOIL FROM 7 TO 14 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 7 TO 18 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. BEDROCK IS AT 18 INCHES."|"542047"|"542047:m:458697"
|"Nontechnical description"|"AGR"|"061112"|"Weikert soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"542047"|"542047:m:458696"
|"Nontechnical description"|"SO5"|"PA0084"|"THE WHARTON SERIES CONSISTS OF DEEP, MODERATELY WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE AND SILTSTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 9 INCHES THICK. THE SUBSOIL FROM 9 TO 22 IN. IS YELLOWISH BROWN SILT LOAM AND SILTY CLAY LOAM, FROM 22 TO 31 IN. IS BROWN SILT LOAM AND FROM 31 TO 46 IN. IS DARK YELLOWISH BROWN SILTY CLAY LOAM. THE SUBSTRATUM FROM 46 TO 60 INCHES IS BROWN SHALY SILTY CLAY LOAM."|"542048"|"542048:m:458698"
|"Nontechnical description"|"AGR"|"061113"|"Wharton soils make up 85 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is high.  It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 3e."|"542048"|"542048:m:458699"
|"Nontechnical description"|"AGR"|"06135"|"Clymer soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541979"|"541979:m:458544"
|"Nontechnical description"|"SO5"|"PA0058"|"THE CLYMER SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A VERY DARK GRAYISH BROWN CHANNERY LOAM SURFACE LAYER ABOUT 8 INCHES THICK. THE SUBSOIL BETWEEN 8 AND 36 INCHES IS YELLOWISH BROWN AND STRONG BROWN CHANNERY LOAM. THE SUBSTRATUM FROM 36 TO 50 INCHES IS YELLOWISH BROWN VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT ABOUT 50 INCHES."|"541979"|"541979:m:458545"
|"Nontechnical description"|"SO5"|"PA0059"|"THE CLYMER SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A VERY DARK GRAYISH BROWN VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER ABOUT 8 INCHES THICK. THE SUBSOIL BETWEEN 8 AND 36 INCHES IS YELLOWISH BROWN AND STRONG BROWN FRIABLE CHANNERY LOAM. THE SUBSTRATUM FROM 36 TO 50 INCHES IS YELLOWISH-BROWN VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT ABOUT 50 INCHES."|"541980"|"541980:m:458546"
|"Nontechnical description"|"AGR"|"06136"|"Clymer soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s."|"541980"|"541980:m:458547"
|"Nontechnical description"|"SO5"|"PA0059"|"THE CLYMER SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A VERY DARK GRAYISH BROWN VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER ABOUT 8 INCHES THICK. THE SUBSOIL BETWEEN 8 AND 36 INCHES IS YELLOWISH BROWN AND STRONG BROWN FRIABLE CHANNERY LOAM. THE SUBSTRATUM FROM 36 TO 50 INCHES IS YELLOWISH-BROWN VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT ABOUT 50 INCHES."|"541981"|"541981:m:458548"
|"Nontechnical description"|"AGR"|"06137"|"Clymer soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s."|"541981"|"541981:m:458549"
|"Nontechnical description"|"AGR"|"06138"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e.

 Opequon soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541982"|"541982:m:458551"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541982"|"541982:m:458550"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541983"|"541983:m:458553"
|"Nontechnical description"|"AGR"|"06140"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e.

 Opequon soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541983"|"541983:m:458554"
|"Nontechnical description"|"AGR"|"06142"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e.

 Opequon soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"541984"|"541984:m:458557"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541984"|"541984:m:458556"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541985"|"541985:m:458559"
|"Nontechnical description"|"AGR"|"06144"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e.

 Weikert soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"541985"|"541985:m:458560"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541986"|"541986:m:458562"
|"Nontechnical description"|"AGR"|"06146"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e.

 Weikert soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541986"|"541986:m:458563"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541987"|"541987:m:458565"
|"Nontechnical description"|"AGR"|"06148"|"Edom soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e.

 Weikert soils make up 20 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is somewhat excessively drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"541987"|"541987:m:458566"
|"Nontechnical description"|"SO5"|"PA0104"|"THE EDOM SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILTY CLAY LOAM SURFACE LAYER 8 INCHES THICK. THE SUBSOIL FROM 8 TO 36 INCHES IS REDDISH BROWN AND YELLOWISH BROWN SILTY CLAY AND CLAY. THE SUBSTRATUM FROM 36 TO 46 INCHES IS REDDISH BROWN VERY SHALY SILTY CLAY. FRACTURED BEDROCK IS AT 46 INCHES. SLOPES RANGE FROM 0 TO 45 PERCENT."|"541988"|"541988:m:458568"
|"Nontechnical description"|"AGR"|"06150"|"Edom soils make up 50 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is low and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7e.

 Weikert soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"541988"|"541988:m:458569"
|"Nontechnical description"|"SO5"|"PA0105"|"THE ELLIBER SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN VERY CHANNERY SILT LOAM SURFACE LAYER 9 INCHES THICK. THE SUBSOIL FROM 9 TO 35 INCHES IS BROWNISH YELLOW AND YELLOWISH BROWN EXTREMELY CHANNERY SILT LOAM, FROM 35 TO 47 INCHES IS YELLOWISH BROWN EXTREMELY CHANNERY LOAM, AND FROM 47 TO 70 INCHES IS YELLOWISH BROWN VERY CLAY LOAM."|"541989"|"541989:m:458571"
|"Nontechnical description"|"AGR"|"06152"|"Elliber soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4s."|"541989"|"541989:m:458572"
|"Nontechnical description"|"AGR"|"06153"|"Elliber soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s."|"541990"|"541990:m:458574"
|"Nontechnical description"|"SO5"|"PA0105"|"THE ELLIBER SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN VERY CHANNERY SILT LOAM SURFACE LAYER 9 INCHES THICK. THE SUBSOIL FROM 9 TO 35 INCHES IS BROWNISH YELLOW AND YELLOWISH BROWN EXTREMELY CHANNERY SILT LOAM, FROM 35 TO 47 INCHES IS YELLOWISH BROWN EXTREMELY CHANNERY LOAM, AND FROM 47 TO 70 INCHES IS YELLOWISH BROWN VERY CLAY LOAM."|"541990"|"541990:m:458573"
|"Nontechnical description"|"SO5"|"WV0018"|"THE ERNEST SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS FORMED IN COLLUVIUM FROM SHALE, SILTSTONE AND SOME SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK GRAYISH-BROWN SILT LOAM SURFACE LAYER, 7 INCHES THICK. THE UPPER 20 INCHES OF THE SUBSOIL IS STRONG BROWN SILT LOAM OR SILTY CLAY LOAM AND YELLOWISH-BROWN SILTY CLAY LOAM THAT IS MOTTLED IN THE LOWER PART. THE LOWER 20 INCHES IS A YELLOWISH-BROWN CHANNERY SILT LOAM FRAGIPAN THAT IS FIRM, BRITTLE AND MOTTLED. THE SUBSTRATUM FROM 47 TO 60 INCHES IS LIGHT BROWNISH-GRAY SILT LOAM."|"541991"|"541991:m:458575"
|"Nontechnical description"|"AGR"|"06154"|"Ernest soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"541991"|"541991:m:458576"
|"Nontechnical description"|"AGR"|"06155"|"Ernest soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 22 to 32 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 3e."|"541992"|"541992:m:458578"
|"Nontechnical description"|"SO5"|"WV0018"|"THE ERNEST SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS FORMED IN COLLUVIUM FROM SHALE, SILTSTONE AND SOME SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK GRAYISH-BROWN SILT LOAM SURFACE LAYER, 7 INCHES THICK. THE UPPER 20 INCHES OF THE SUBSOIL IS STRONG BROWN SILT LOAM OR SILTY CLAY LOAM AND YELLOWISH-BROWN SILTY CLAY LOAM THAT IS MOTTLED IN THE LOWER PART. THE LOWER 20 INCHES IS A YELLOWISH-BROWN CHANNERY SILT LOAM FRAGIPAN THAT IS FIRM, BRITTLE AND MOTTLED. THE SUBSTRATUM FROM 47 TO 60 INCHES IS LIGHT BROWNISH-GRAY SILT LOAM."|"541992"|"541992:m:458577"
|"Nontechnical description"|"AGR"|"06156"|"Hazleton soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s.

 Dekalb soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s."|"541993"|"541993:m:458579"
|"Nontechnical description"|"SO5"|"PA0203"|"THE DEKALB SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED MAINLY FROM SANDSTONE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAY VERY STONY OR EXTREMELY STONY SANDY LOAM SURFACE LAYER 2 INCHES THICK OVER 6 INCHES OF LIGHT YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSOIL FROM 8 TO 29 INCHES IS YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 29 TO 34 INCHES IS STRONG BROWN VERY FLAGGY LOAM. SANDSTONE IS AT A DEPTH OF 34 INCHES."|"541993"|"541993:m:458581"
|"Nontechnical description"|"AGR"|"06158"|"Hazleton soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s.

 Dekalb soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s."|"541994"|"541994:m:458582"
|"Nontechnical description"|"SO5"|"PA0203"|"THE DEKALB SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED MAINLY FROM SANDSTONE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAY VERY STONY OR EXTREMELY STONY SANDY LOAM SURFACE LAYER 2 INCHES THICK OVER 6 INCHES OF LIGHT YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSOIL FROM 8 TO 29 INCHES IS YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 29 TO 34 INCHES IS STRONG BROWN VERY FLAGGY LOAM. SANDSTONE IS AT A DEPTH OF 34 INCHES."|"541994"|"541994:m:458584"
|"Nontechnical description"|"SO5"|"MD0004"|"THE HAGERSTOWN SERIES CONSISTS OF DEEP, WELL DRAINED, REDDISH SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM HARD, FAIRLY PURE LIMESTONE. TYPICALLY THESE SOILS HAVE AN 8 INCH PLOW LAYER OF BROWN OR DARK BROWN SILT LOAM. THE MATERIAL BELOW THIS DEPTH AND EXTENDING RATHER UNIFORMLY TO BEDROCK IS GENERALLY YELLOWISH RED CLAY OR SILTY CLAY, WITH LIMESTONE FRAGMENTS COMMON IN THE LOWER SUBSOIL AND IN THE SUBSTRATUM. SINK HOLES OCCUR IN SOME PLACES AND LIMESTONE ROCK OUTCROPS ARE COMMON."|"541995"|"541995:m:458585"
|"Nontechnical description"|"AGR"|"06160"|"Hagerstown soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is greater than 48 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541995"|"541995:m:458586"
|"Nontechnical description"|"SO5"|"MD0004"|"THE HAGERSTOWN SERIES CONSISTS OF DEEP, WELL DRAINED, REDDISH SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM HARD, FAIRLY PURE LIMESTONE. TYPICALLY THESE SOILS HAVE AN 8 INCH PLOW LAYER OF BROWN OR DARK BROWN SILT LOAM. THE MATERIAL BELOW THIS DEPTH AND EXTENDING RATHER UNIFORMLY TO BEDROCK IS GENERALLY YELLOWISH RED CLAY OR SILTY CLAY, WITH LIMESTONE FRAGMENTS COMMON IN THE LOWER SUBSOIL AND IN THE SUBSTRATUM. SINK HOLES OCCUR IN SOME PLACES AND LIMESTONE ROCK OUTCROPS ARE COMMON."|"541996"|"541996:m:458587"
|"Nontechnical description"|"AGR"|"06161"|"Hagerstown soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 48 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541996"|"541996:m:458588"
|"Nontechnical description"|"AGR"|"061"|"Hagerstown soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is greater than 48 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"541997"|"541997:m:458589"
|"Nontechnical description"|"AGR"|"06162"|"Hagerstown soils make up 75 percent of the map unit. Rock Outcrops are within this map unit. This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 48 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is very high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"541998"|"541998:m:458591"
|"Nontechnical description"|"SO5"|"MD0004"|"THE HAGERSTOWN SERIES CONSISTS OF DEEP, WELL DRAINED, REDDISH SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM HARD, FAIRLY PURE LIMESTONE. TYPICALLY THESE SOILS HAVE AN 8 INCH PLOW LAYER OF BROWN OR DARK BROWN SILT LOAM. THE MATERIAL BELOW THIS DEPTH AND EXTENDING RATHER UNIFORMLY TO BEDROCK IS GENERALLY YELLOWISH RED CLAY OR SILTY CLAY, WITH LIMESTONE FRAGMENTS COMMON IN THE LOWER SUBSOIL AND IN THE SUBSTRATUM. SINK HOLES OCCUR IN SOME PLACES AND LIMESTONE ROCK OUTCROPS ARE COMMON."|"541998"|"541998:m:458590"
|"Nontechnical description"|"SO5"|"PA0080"|"THE HAZLETON SERIES CONSISTS OF VERY DEEP AND DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN SANDY LOAM SURFACE LAYER, 6 INCHES THICK. THE SUBSOIL BETWEEN 6 AND 32 INCHES IS REDDISH-YELLOW TO STRONG BROWN CHANNERY AND VERY CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 32 TO 56 INCHES IS REDDISH-YELLOW VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT A DEPTH OF 56 INCHES."|"541999"|"541999:m:458592"
|"Nontechnical description"|"AGR"|"06163"|"Hazleton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"541999"|"541999:m:458593"
|"Nontechnical description"|"AGR"|"06164"|"Hazleton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542000"|"542000:m:458595"
|"Nontechnical description"|"SO5"|"PA0080"|"THE HAZLETON SERIES CONSISTS OF VERY DEEP AND DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN SANDY LOAM SURFACE LAYER, 6 INCHES THICK. THE SUBSOIL BETWEEN 6 AND 32 INCHES IS REDDISH-YELLOW TO STRONG BROWN CHANNERY AND VERY CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 32 TO 56 INCHES IS REDDISH-YELLOW VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT A DEPTH OF 56 INCHES."|"542000"|"542000:m:458594"
|"Nontechnical description"|"SO5"|"PA0080"|"THE HAZLETON SERIES CONSISTS OF VERY DEEP AND DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY, THESE SOILS HAVE A DARK BROWN SANDY LOAM SURFACE LAYER, 6 INCHES THICK. THE SUBSOIL BETWEEN 6 AND 32 INCHES IS REDDISH-YELLOW TO STRONG BROWN CHANNERY AND VERY CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 32 TO 56 INCHES IS REDDISH-YELLOW VERY CHANNERY SANDY LOAM. SANDSTONE BEDROCK IS AT A DEPTH OF 56 INCHES."|"542001"|"542001:m:458596"
|"Nontechnical description"|"AGR"|"06165"|"Hazleton soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is greater than 42 inches to bedrock. It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542001"|"542001:m:458597"
|"Nontechnical description"|"SO5"|"PA0203"|"THE DEKALB SERIES CONSISTS OF MODERATELY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED MAINLY FROM SANDSTONE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAY VERY STONY OR EXTREMELY STONY SANDY LOAM SURFACE LAYER 2 INCHES THICK OVER 6 INCHES OF LIGHT YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSOIL FROM 8 TO 29 INCHES IS YELLOWISH BROWN CHANNERY SANDY LOAM. THE SUBSTRATUM FROM 29 TO 34 INCHES IS STRONG BROWN VERY FLAGGY LOAM. SANDSTONE IS AT A DEPTH OF 34 INCHES."|"542002"|"542002:m:458598"
|"Nontechnical description"|"AGR"|"06166"|"Hazleton soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is very low.  The depth to a restrictive feature is 40 inches bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s.
 Dekalb soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is very low.  The depth to a restrictive feature is 20 to 40 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is rapid.  Available water capacity is low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s."|"542002"|"542002:m:458599"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542003"|"542003:m:458601"
|"Nontechnical description"|"AGR"|"06168"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"542003"|"542003:m:458602"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542004"|"542004:m:458603"
|"Nontechnical description"|"AGR"|"06169"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542004"|"542004:m:458604"
|"Nontechnical description"|"AGR"|"06170"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542005"|"542005:m:458606"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542005"|"542005:m:458605"
|"Nontechnical description"|"AGR"|"06171"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"542006"|"542006:m:458608"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542006"|"542006:m:458607"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542007"|"542007:m:458609"
|"Nontechnical description"|"AGR"|"06172"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542007"|"542007:m:458610"
|"Nontechnical description"|"AGR"|"06173"|"Hublersburg soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is moderate.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542008"|"542008:m:458612"
|"Nontechnical description"|"SO5"|"PA0116"|"THE HUBLERSBURG SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIALS WEATHERED FROM CHERTY LIMESTONE. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN CHERTY SILT LOAM SURFACE LAYER 8 INCHES THICK AND A SUBSURFACE LAYER FROM 8 TO 14 INCHES OF LIGHT YELLOWISH BROWN CHERTY SILT LOAM. THE SUBSOIL FROM 14 TO 21 INCHES IS YELLOWISH BROWN SILTY CLAY LOAM, FROM 21 TO 46 INCHES IT IS CHERTY SILTY CLAY, FROM 46 TO 65 INCHES IT IS SILTY CLAY AND FROM 65 TO 74 INCHES IT IS CLAY."|"542008"|"542008:m:458611"
|"Nontechnical description"|"SO5"|"PA0045"|"THE KLINESVILLE SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK REDDISH BROWN VERY SHALY SILT LOAM SURFACE LAYER 5 INCHES THICK. THE SUBSOIL FROM 5 TO 15 INCHES IS REDDISH BROWN VERY SHALY SILT LOAM. THE SUBSTRATUM FROM 15 TO 19 INCHES IS WEAK RED WEATHERED SHALE FRAGMENTS. BEDROCK IS AT 19 INCHES."|"542009"|"542009:m:458613"
|"Nontechnical description"|"AGR"|"06174"|"Klinesville soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542009"|"542009:m:458614"
|"Nontechnical description"|"SO5"|"PA0045"|"THE KLINESVILLE SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK REDDISH BROWN VERY SHALY SILT LOAM SURFACE LAYER 5 INCHES THICK. THE SUBSOIL FROM 5 TO 15 INCHES IS REDDISH BROWN VERY SHALY SILT LOAM. THE SUBSTRATUM FROM 15 TO 19 INCHES IS WEAK RED WEATHERED SHALE FRAGMENTS. BEDROCK IS AT 19 INCHES."|"542010"|"542010:m:458615"
|"Nontechnical description"|"AGR"|"06175"|"Klinesville soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"542010"|"542010:m:458616"
|"Nontechnical description"|"AGR"|"06176"|"Laidig soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 30 to 41 inches.  Major component is not a hydric soil.  Land capability class 7s."|"542011"|"542011:m:458617"
|"Nontechnical description"|"SO5"|"WV0052"|"THE LAIDIG SERIES CONSISTS OF VERY DEEP, WELL-DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY, THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH-BROWN EXTRMEELY STONY LOAM SURFACE LAYER, 2 INCHES THICK, AND A YELLOWISH-BROWN SUBSURFACE LAYER, 6 INCHES THICK. THE SUBSOIL FROM 8 TO 14 INCHES IS CHANNERY LOAM AND FROM 14 TO 37 INCHES IS CHANNERY SANDY CLAY LOAM. FROM 37 TO 80 INCHES IS A CHANNERY SANDY CLAY LOAM FRAGIPAN THAT IS VERY FIRM AND BRITTLE."|"542011"|"542011:m:458618"
|"Nontechnical description"|"SO5"|"WV0001"|"THE LAIDIG SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED MAINLY FROM SANDSTONE AND SHALE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH BROWN CHANNERY LOAM SURFACE LAYER 2 INCHES THICK, A YELLOWISH BROWN CHANNERY LOAM SUBSURFACE LAYER TO 8 INCHES. THE SUBSOIL, FROM 8 TO 14 INCHES IS YELLOWISH BROWN CHANNERY LOAM AND FROM 14 TO 37 INCHES IS STRONG BROWN CHANNERY SANDY CLAY LOAM. FROM 37 TO 80 INCHES IS A STRONG BROWN CHANNERY SANDY CLAY LOAM FRAGIPAN THAT IS VERY FIRM AND BRITTLE."|"542012"|"542012:m:458619"
|"Nontechnical description"|"AGR"|"06177"|"Laidig soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 30 to 41 inches.  Major component is not a hydric soil.  Land capability class 2e."|"542012"|"542012:m:458620"
|"Nontechnical description"|"AGR"|"06178"|"Laidig soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 30 to 41 inches.  Major component is not a hydric soil.  Land capability class 3e."|"542013"|"542013:m:458622"
|"Nontechnical description"|"SO5"|"WV0001"|"THE LAIDIG SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED MAINLY FROM SANDSTONE AND SHALE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH BROWN CHANNERY LOAM SURFACE LAYER 2 INCHES THICK, A YELLOWISH BROWN CHANNERY LOAM SUBSURFACE LAYER TO 8 INCHES. THE SUBSOIL, FROM 8 TO 14 INCHES IS YELLOWISH BROWN CHANNERY LOAM AND FROM 14 TO 37 INCHES IS STRONG BROWN CHANNERY SANDY CLAY LOAM. FROM 37 TO 80 INCHES IS A STRONG BROWN CHANNERY SANDY CLAY LOAM FRAGIPAN THAT IS VERY FIRM AND BRITTLE."|"542013"|"542013:m:458621"
|"Nontechnical description"|"AGR"|"06179"|"Laidig soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 30 to 41 inches.  Major component is not a hydric soil.  Land capability class 4e."|"542014"|"542014:m:458624"
|"Nontechnical description"|"SO5"|"WV0001"|"THE LAIDIG SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM DERIVED MAINLY FROM SANDSTONE AND SHALE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH BROWN CHANNERY LOAM SURFACE LAYER 2 INCHES THICK, A YELLOWISH BROWN CHANNERY LOAM SUBSURFACE LAYER TO 8 INCHES. THE SUBSOIL, FROM 8 TO 14 INCHES IS YELLOWISH BROWN CHANNERY LOAM AND FROM 14 TO 37 INCHES IS STRONG BROWN CHANNERY SANDY CLAY LOAM. FROM 37 TO 80 INCHES IS A STRONG BROWN CHANNERY SANDY CLAY LOAM FRAGIPAN THAT IS VERY FIRM AND BRITTLE."|"542014"|"542014:m:458623"
|"Nontechnical description"|"SO5"|"WV0052"|"THE LAIDIG SERIES CONSISTS OF VERY DEEP, WELL-DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY, THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH-BROWN EXTRMEELY STONY LOAM SURFACE LAYER, 2 INCHES THICK, AND A YELLOWISH-BROWN SUBSURFACE LAYER, 6 INCHES THICK. THE SUBSOIL FROM 8 TO 14 INCHES IS CHANNERY LOAM AND FROM 14 TO 37 INCHES IS CHANNERY SANDY CLAY LOAM. FROM 37 TO 80 INCHES IS A CHANNERY SANDY CLAY LOAM FRAGIPAN THAT IS VERY FIRM AND BRITTLE."|"542015"|"542015:m:458625"
|"Nontechnical description"|"AGR"|"06180"|"Laidig soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 30 to 41 inches.  Major component is not a hydric soil.  Land capability class 7s."|"542015"|"542015:m:458626"
|"Nontechnical description"|"AGR"|"06181"|"Leetonia soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is 40 to 48 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s."|"542016"|"542016:m:458628"
|"Nontechnical description"|"SO5"|"VA0022"|"THE LEETONIA SERIES CONSISTS OF DEEP, WELL DRAINED TO EXCESSIVELY DRAINED SOILS ON UPLANDS. THEY FORMED IN RESIDUUM. TYPICALLY THESE SOILS HAVE A DARK GRAY VERY OR EXTREMELY STONY LOAMY SAND SURFACE LAYER 7 INCHES THICK. THE SUBSOIL LAYERS FROM 7 TO 20 INCHES ARE DARK BROWN GRAVELLY LOAMY SAND AND BROWNISH YELLOW VERY GRAVELLY SAND. THE SUBSTRATUM FROM 20 INCHES TO BEDROCK AT 45 INCHES IS OLIVE YELLOW VERY GRAVELLY SAND. SLOPES RANGE FROM 0 TO 60 PERCENT."|"542016"|"542016:m:458627"
|"Nontechnical description"|"SO5"|"PA0031"|"THE MECKESVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM OR GLACIAL TILL. TYPICALLY THESE SOILS HAVE A LOAM SURFACE LAYER 7 INCHES THICK THAT IS DARK REDDISH BROWN AND REDDISH BROWN. THE SUBSOIL FROM 7 TO 14 INCHES IS REDDISH BROWN CLAY LOAM, FROM 14 TO 31 INCHES IS REDDISH BROWN AND DUSTY RED LOAM AND GRAVELLY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 31 TO 70 INCHES IS WEAK RED GRAVELLY LOAM AND GRAVELLY CLAY LOAM. THE SUBSTRATUM FROM 70 TO 96 INCHES IS WEAK RED GRAVELLY LOAM."|"542017"|"542017:m:458629"
|"Nontechnical description"|"AGR"|"06182"|"Meckesville soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is high and shrink swell potential is low.   The top of the seasonal high water table ranges from 36 to 72 inches.  Major component is not a hydric soil.  Land capability class 3e."|"542017"|"542017:m:458630"
|"Nontechnical description"|"SO5"|"PA0032"|"THE MECKESVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM OR GLACIAL TILL. TYPICALLY THESE SOILS HAVE A VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER 7 INCHES THICK THAT IS DARK REDDISH BROWN AND REDDISH BROWN. THE SUBSOIL LAYERS FROM 7 TO 31 INCHES ARE MAINLY REDDISH BROWN WITH TEXTURES OF CLAY LOAM, LOAM, AND GRAVELLY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 31 TO 70 INCHES IS GRAVELLY LOAM AND CLAY LOAM. THE SUBSTRATUM FROM 70 TO 96 INCHES IS GRAVELLY LOAM."|"542018"|"542018:m:458631"
|"Nontechnical description"|"AGR"|"06183"|"Meckesville soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is high and shrink swell potential is low.   The top of the seasonal high water table ranges from 36 to 72 inches.  Major component is not a hydric soil.  Land capability class 6s."|"542018"|"542018:m:458632"
|"Nontechnical description"|"AGR"|"06184"|"Meckesville soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 28 to 42 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is high and shrink swell potential is low.   The top of the seasonal high water table ranges from 36 to 72 inches.  Major component is not a hydric soil.  Land capability class 6s."|"542019"|"542019:m:458633"
|"Nontechnical description"|"SO5"|"PA0032"|"THE MECKESVILLE SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIUM OR GLACIAL TILL. TYPICALLY THESE SOILS HAVE A VERY STONY OR EXTREMELY STONY LOAM SURFACE LAYER 7 INCHES THICK THAT IS DARK REDDISH BROWN AND REDDISH BROWN. THE SUBSOIL LAYERS FROM 7 TO 31 INCHES ARE MAINLY REDDISH BROWN WITH TEXTURES OF CLAY LOAM, LOAM, AND GRAVELLY LOAM. A VERY FIRM AND BRITTLE FRAGIPAN FROM 31 TO 70 INCHES IS GRAVELLY LOAM AND CLAY LOAM. THE SUBSTRATUM FROM 70 TO 96 INCHES IS GRAVELLY LOAM."|"542019"|"542019:m:458634"
|"Nontechnical description"|"SO5"|"WV0006"|"THE MONONGAHELA SERIES CONSISTS OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON TERRACES. THEY FORMED IN OLD ALLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 7 INCHES THICK OVER 5 INCHES OF YELLOWISH BROWN SILT LOAM. THE SUBSOIL FROM 12 TO 22 INCHES IS YELLOWISH BROWN SILT LOAM. FROM 22 TO 52 INCHES IS A FIRM TO VERY FIRM FRAGIPAN THAT IS YELLOWISH BROWN AND LIGHT YELLOWISH BROWN LOAM. THE SUBSTRATUM FROM 52 TO 60 INCHES IS STRONG BROWN AND LIGHT GRAY CLAY LOAM."|"542020"|"542020:m:458635"
|"Nontechnical description"|"AGR"|"06185"|"Monongahela soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  The depth to a restrictive feature is 18 to 30 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is slow.  Available water capacity is moderate and shrink swell potential is low.   The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"542020"|"542020:m:458636"
|"Nontechnical description"|"AGR"|"06186"|"Morrison soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"542021"|"542021:m:458638"
|"Nontechnical description"|"SO5"|"PA0125"|"THE MORRISON SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS HAVE A BROWNISH, LOAMY SAND AND SANDY LOAM SURFACE LAYER 14 INCHES THICK. THE SUBSOIL FROM 14 TO 53 INCHES IS STRONG BROWN AND YELLOWISH RED SANDY LOAM, CHANNERY CLAY LOAM, AND CHANNERY SANDY CLAY LOAM. THE SUBSTRATUM FROM 53 TO 74 INCHES IS STRONG BROWN CHANNERY SANDY LOAM."|"542021"|"542021:m:458637"
|"Nontechnical description"|"AGR"|"06187"|"Morrison soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542022"|"542022:m:458640"
|"Nontechnical description"|"SO5"|"PA0125"|"THE MORRISON SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS HAVE A BROWNISH, LOAMY SAND AND SANDY LOAM SURFACE LAYER 14 INCHES THICK. THE SUBSOIL FROM 14 TO 53 INCHES IS STRONG BROWN AND YELLOWISH RED SANDY LOAM, CHANNERY CLAY LOAM, AND CHANNERY SANDY CLAY LOAM. THE SUBSTRATUM FROM 53 TO 74 INCHES IS STRONG BROWN CHANNERY SANDY LOAM."|"542022"|"542022:m:458639"
|"Nontechnical description"|"SO5"|"PA0125"|"THE MORRISON SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS HAVE A BROWNISH, LOAMY SAND AND SANDY LOAM SURFACE LAYER 14 INCHES THICK. THE SUBSOIL FROM 14 TO 53 INCHES IS STRONG BROWN AND YELLOWISH RED SANDY LOAM, CHANNERY CLAY LOAM, AND CHANNERY SANDY CLAY LOAM. THE SUBSTRATUM FROM 53 TO 74 INCHES IS STRONG BROWN CHANNERY SANDY LOAM."|"542023"|"542023:m:458641"
|"Nontechnical description"|"AGR"|"06188"|"Morrison soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542023"|"542023:m:458642"
|"Nontechnical description"|"AGR"|"06189"|"Morrison soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s."|"542024"|"542024:m:458644"
|"Nontechnical description"|"SO5"|"PA0126"|"THE MORRISON SERIES CONSISTS OF DEEP WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS HAVE A BROWNISH, VERY STONY, LOAMY SAND AND SANDY LOAM SURFACE LAYER 14 INCHES THICK. THE SUBSOIL FROM 14 TO 53 INCHES IS STRONG BROWN AND YELLOWISH RED SANDY LOAM, CHANNERY CLAY LOAM, AND CHANNERY SANDY CLAY LOAM. THE SUBSTRATUM FROM 53 TO 74 INCHES IS STRONG BROWN CHANNERY SANDY LOAM."|"542024"|"542024:m:458643"
|"Nontechnical description"|"SO5"|"PA0126"|"THE MORRISON SERIES CONSISTS OF DEEP WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS HAVE A BROWNISH, VERY STONY, LOAMY SAND AND SANDY LOAM SURFACE LAYER 14 INCHES THICK. THE SUBSOIL FROM 14 TO 53 INCHES IS STRONG BROWN AND YELLOWISH RED SANDY LOAM, CHANNERY CLAY LOAM, AND CHANNERY SANDY CLAY LOAM. THE SUBSTRATUM FROM 53 TO 74 INCHES IS STRONG BROWN CHANNERY SANDY LOAM."|"542025"|"542025:m:458645"
|"Nontechnical description"|"AGR"|"06190"|"Morrison soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6s."|"542025"|"542025:m:458646"
|"Nontechnical description"|"SO5"|"WV0028"|"THE MURRILL SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN CHANNERY LOAM SURFACE LAYER 9 INCHES THICK OVER 6 INCHES OF BROWN CHANNERY LOAM. THE SUBSOIL FROM 15 TO 21 INCHES IS YELLOWISH BROWN CHANNERY SILTY CLAY LOAM, FROM 21 TO 60 INCHES IS DARK BROWN AND STRONG BROWN CHANNERY SANDY CLAY LOAM, AND FROM 60 TO 80 INCHES IS REDDISH BROWN CLAY LOAM."|"542026"|"542026:m:458647"
|"Nontechnical description"|"AGR"|"06191"|"Murrill soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 2e."|"542026"|"542026:m:458648"
|"Nontechnical description"|"SO5"|"WV0028"|"THE MURRILL SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN CHANNERY LOAM SURFACE LAYER 9 INCHES THICK OVER 6 INCHES OF BROWN CHANNERY LOAM. THE SUBSOIL FROM 15 TO 21 INCHES IS YELLOWISH BROWN CHANNERY SILTY CLAY LOAM, FROM 21 TO 60 INCHES IS DARK BROWN AND STRONG BROWN CHANNERY SANDY CLAY LOAM, AND FROM 60 TO 80 INCHES IS REDDISH BROWN CLAY LOAM."|"542027"|"542027:m:458649"
|"Nontechnical description"|"AGR"|"06192"|"Murrill soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542027"|"542027:m:458650"
|"Nontechnical description"|"SO5"|"WV0028"|"THE MURRILL SERIES CONSISTS OF VERY DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN COLLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK YELLOWISH BROWN CHANNERY LOAM SURFACE LAYER 9 INCHES THICK OVER 6 INCHES OF BROWN CHANNERY LOAM. THE SUBSOIL FROM 15 TO 21 INCHES IS YELLOWISH BROWN CHANNERY SILTY CLAY LOAM, FROM 21 TO 60 INCHES IS DARK BROWN AND STRONG BROWN CHANNERY SANDY CLAY LOAM, AND FROM 60 TO 80 INCHES IS REDDISH BROWN CLAY LOAM."|"542028"|"542028:m:458651"
|"Nontechnical description"|"AGR"|"06193"|"Murrill soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542028"|"542028:m:458652"
|"Nontechnical description"|"AGR"|"06194"|"Newark soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is very high.  It is somewhat poorly drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is high and shrink swell potential is low. This soil is subject to occasional flooding and is not ponded.  The top of the seasonal high water table ranges from 6 to 18 inches.  Major component is not a hydric soil.  Land capability class 2w."|"542029"|"542029:m:458654"
|"Nontechnical description"|"SO5"|"KY0003"|"THE NEWARK SERIES CONSISTS OF DEEP, SOMEWHAT POORLY DRAINED SOILS ON FLOOD PLAINS. THEY FORMED IN ALLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A BROWN SILT LOAM SURFACE LAYER 9 INCHES THICK. THE SUBSOIL FROM 9 TO 32 INCHES IS SILT LOAM THAT IS BROWN IN THE UPPER PART AND LIGHT BROWNISH GRAY IN THE LOWER PART. THE SUBSTRATUM FROM 32 TO 60 INCHES OR MORE IS LIGHT BROWNISH GRAY AND BROWN SILT LOAM. THE SUBSOIL AND SUBSTRATUM ARE MOTTLED IN SHADES OF GRAY AND BROWN."|"542029"|"542029:m:458653"
|"Nontechnical description"|"AGR"|"06197"|"Soil ROCK OUTCROP is 0 - inches to bedrock. Permeability is VERY SLOW and available water holding capacity is VERY LOW. A water table when present is >6 - feet. The soil productivity is NOT SUITED TO CROPLAND and the capability subclass is NONE."|"542030"|"542030:m:458657"
|"Nontechnical description"|"AGR"|"06195"|"Opequon soils make up 60 percent of the map unit. Areas of Hagerstown soils and rock outcrops make up the rest of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7e."|"542030"|"542030:m:458655"
|"Nontechnical description"|"SO5"|"WV0024"|"THE OPEQUON SERIES CONSISTS OF SHALLOW, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE. TYPICALLY THESE SOILS HAVE A BROWN SILTY CLAY SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 11 INCHES IS YELLOWISH RED CLAY AND FROM 11 TO 16 INCHES IS RED CLAY. LIMESTONE BEDROCK IS AT A DEPTH OF 16 INCHES."|"542031"|"542031:m:458658"
|"Nontechnical description"|"AGR"|"06198"|"Opequon soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542031"|"542031:m:458659"
|"Nontechnical description"|"AGR"|"06199"|"Opequon soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is medium.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542032"|"542032:m:458661"
|"Nontechnical description"|"SO5"|"WV0024"|"THE OPEQUON SERIES CONSISTS OF SHALLOW, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE. TYPICALLY THESE SOILS HAVE A BROWN SILTY CLAY SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 11 INCHES IS YELLOWISH RED CLAY AND FROM 11 TO 16 INCHES IS RED CLAY. LIMESTONE BEDROCK IS AT A DEPTH OF 16 INCHES."|"542032"|"542032:m:458660"
|"Nontechnical description"|"SO5"|"WV0024"|"THE OPEQUON SERIES CONSISTS OF SHALLOW, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM LIMESTONE. TYPICALLY THESE SOILS HAVE A BROWN SILTY CLAY SURFACE LAYER 6 INCHES THICK. THE SUBSOIL FROM 6 TO 11 INCHES IS YELLOWISH RED CLAY AND FROM 11 TO 16 INCHES IS RED CLAY. LIMESTONE BEDROCK IS AT A DEPTH OF 16 INCHES."|"542033"|"542033:m:458662"
|"Nontechnical description"|"AGR"|"061100"|"Opequon soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is high.  The depth to a restrictive feature is 12 to 20 inches to bedrock (lithic). It is well drained.  The slowest permeability within 60 inches is moderately slow.  Available water capacity is very low and shrink swell potential is high.    The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 6e."|"542033"|"542033:m:458663"
|"Nontechnical description"|"SOI"|"091meb"|"Made land, shale and sandstone, sloping are areas of soil altered by earth moving activities in formerly sandstone and shale soils. Soils usually contain many rock fragments, and are silty to sandy and compacted."|"542034"|"542034:m:458664"
|"Nontechnical description"|"AGR"|"061"|"This miscellaneous land type has variable properties that require onsite investigations to determine soil properties and suitability for most all uses."|"542034"|"542034:m:458665"
|"Nontechnical description"|"SO5"|"WV0020"|"THE PHILO SERIES CONSISTS OF DEEP OR VERY DEEP, MODERATELY WELL DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN RECENT ALLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK BROWN SILT LOAM SURFACE LAYER 6 INCHES THICK. THE SILT LOAM SUBSOIL FROM 6 TO 22 INCHES IS DARK YELLOWISH BROWN AND BROWN. THE SUBSTRATUM FROM 22 TO 32 INCHES IS GRAY SILT LOAM FROM 32 TO 42 INCHES IS GRAY AND STRONG BROWN LOAM, AND FROM 42 TO 60 INCHES IS STRATIFIED SAND AND GRAVEL."|"542035"|"542035:m:458666"
|"Nontechnical description"|"AGR"|"061101"|"Philo soils make up 60 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is moderately well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to occasional flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2w.

 Basher soils make up 30 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  The depth to a restrictive feature is 28 to 35 inches to fragipan. It is moderately well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to occasional flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2w."|"542035"|"542035:m:458667"
|"Nontechnical description"|"SO5"|"NY0231"|"THE BASHER SERIES CONSIST OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN ALLUVIAL DEPOSITS DERIVED FROM REDDISH SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK REDDISH BROWN SURFACE LAYER 9 INCHES THICK. THE SUBSOIL LAYERS FROM 9 TO 27 INCHES ARE DARK REDDISH BROWN AND YELLOWISH BROWN SILT LOAM. THE SUBSTRATUM FROM 27 TO 42 INCHES IS GRAYISH BROWN AND GRAY LOAM AND FROM 42 TO 60 INCHES IT IS VERY DARK GRAY FINE SANDY LOAM. SLOPES RANGE FROM 0 TO 3 PERCENT."|"542035"|"542035:m:458669"
|"Nontechnical description"|"SO5"|"WV0020"|"THE PHILO SERIES CONSISTS OF DEEP OR VERY DEEP, MODERATELY WELL DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN RECENT ALLUVIAL MATERIAL. TYPICALLY THESE SOILS HAVE A DARK BROWN SILT LOAM SURFACE LAYER 6 INCHES THICK. THE SILT LOAM SUBSOIL FROM 6 TO 22 INCHES IS DARK YELLOWISH BROWN AND BROWN. THE SUBSTRATUM FROM 22 TO 32 INCHES IS GRAY SILT LOAM FROM 32 TO 42 INCHES IS GRAY AND STRONG BROWN LOAM, AND FROM 42 TO 60 INCHES IS STRATIFIED SAND AND GRAVEL."|"542036"|"542036:m:458670"
|"Nontechnical description"|"AGR"|"061103"|"Philo soils make up 45 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is moderately well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to rare flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2w.

 Basher soils make up 40 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Prime Farmland.  The runoff class is low.  It is moderately well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to rare flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 24 inches.  Major component is not a hydric soil.  Land capability class 2w."|"542036"|"542036:m:458671"
|"Nontechnical description"|"SO5"|"NY0231"|"THE BASHER SERIES CONSIST OF VERY DEEP, MODERATELY WELL DRAINED SOILS ON FLOODPLAINS. THEY FORMED IN ALLUVIAL DEPOSITS DERIVED FROM REDDISH SANDSTONE, SILTSTONE AND SHALE. TYPICALLY THESE SOILS HAVE A DARK REDDISH BROWN SURFACE LAYER 9 INCHES THICK. THE SUBSOIL LAYERS FROM 9 TO 27 INCHES ARE DARK REDDISH BROWN AND YELLOWISH BROWN SILT LOAM. THE SUBSTRATUM FROM 27 TO 42 INCHES IS GRAYISH BROWN AND GRAY LOAM AND FROM 42 TO 60 INCHES IT IS VERY DARK GRAY FINE SANDY LOAM. SLOPES RANGE FROM 0 TO 3 PERCENT."|"542036"|"542036:m:458673"
|"Nontechnical description"|"AGR"|"061105"|"Purdy soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This soil is on a stream terrace.  The runoff class is very high.  It is poorly drained.  The slowest permeability within 60 inches is very slow.  Available water capacity is high and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 0 to 6 inches.  Major component is a hydric soil.  Land capability class 4w."|"542037"|"542037:m:458675"
|"Nontechnical description"|"SO5"|"WV0034"|"THE PURDY SERIES CONSISTS OF VERY DEEP, POORLY TO VERY POORLY DRAINED SOILS ON TERRACES. THEY FORMED IN SLACK WATER ALLUVIAL DEPOSITS. TYPICALLY THESE SOILS HAVE A MOTTLED DARK GRAYISH BROWN SILT LOAM SURFACE LAYER 9 INCHES THICK. THE MOTTLED SUBSOIL FROM 9 TO 19 INCHES IS GRAY SILTY CLAY LOAM AND FROM 19 TO 42 INCHES IS DARK GRAY SILTY CLAY. THE SUBSTRATUM FROM 42 TO 60 INCHES IS GRAY SILTY CLAY."|"542037"|"542037:m:458674"
|"Nontechnical description"|"AGR"|"061106"|"Raritan soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is medium.  The depth to a restrictive feature is 20 to 28 inches to fragipan. It is well drained.  The slowest permeability within 60 inches is moderate.  Available water capacity is moderate and shrink swell potential is low. This soil is subject to rare flooding and is not ponded.  The top of the seasonal high water table ranges from 18 to 36 inches.  Major component is not a hydric soil.  Land capability class 2e."|"542038"|"542038:m:458677"
|"Nontechnical description"|"SO5"|"PA0040"|"THE RARITAN SERIES CONSISTS OF VERY DEEP, MODERATELY WELL AND SOMEWHAT POORLY DRAINED SOILS ON STREAM TERRACES. THEY FORMED IN STREAM DEPOSITS WASHED FROM UPLANDS UNDERLAIN BY REDDISH SHALE, SILTSTONE AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN SILT LOAM SURFACE LAYER ABOUT 9 INCHES THICK. THE SUBSOIL BETWEEN 9 AND 43 INCHES IS STRONG BROWN REDDISH BROWN FRIABLE TO VERY FIRM SILT LOAM AND CLAY LOAM. THE SUBSTRATUM FROM 43 TO 60 INCHES IS REDDISH BROWN STRATIFIED SAND, SILT AND GRAVEL."|"542038"|"542038:m:458676"
|"Nontechnical description"|"AGR"|"061"|"This miscellaneous land type has variable properties that require onsite investigations to determine soil properties and suitability for most all uses."|"542039"|"542039:m:458679"
|"Nontechnical description"|"SOI"|"400"|"Extremely stony land consists of steep areas of boulders and rocks on mountain sides. The rocks are mainly quartzite. Tree growth is poor and soils under the stone cover are thin or similar to Laidig or Fleetwood."|"542039"|"542039:m:458678"
|"Nontechnical description"|"SO5"|"PA999"|"THESE AREAS ARE MISCELLANEOUS LAND TYPES THAT HAVE NO SOIL OR HIGHLY VARIABLE SOIL PROPERTIES. ONSITE INVESTIGATIONS ARE NEEDED TO DETERMINE THEIR SUITABILITY FOR MOST USES."|"542040"|"542040:m:458680"
|"Nontechnical description"|"AGR"|"061"|"This miscellaneous land type has variable properties that require onsite investigations to determine soil properties and suitability for most all uses."|"542040"|"542040:m:458681"
|"Nontechnical description"|"SO5"|"OH0109"|"THE TYLER SERIES CONSISTS OF DEEP, SOMEWHAT POORLY DRAINED SOILS FORMED IN SILTY SEDIMENTS ON TERRACES. THE SURFACE LAYER IS DARK GRAYISH BROWN SILT LOAM 9 INCHES THICK. THE SUBSURFACE LAYER IS LIGHT YELLOWISH BROWN MOTTLED SILT LOAM 5 INCHES THICK. THE MOTTLED SUBSOIL IS LIGHT BROWNISH GRAY SILTY CLAY LOAM IN UPPER 4 INCHES, YELLOWISH BROWN AND LIGHT YELLOWISH BROWN SILTY CLAY LOAM FRAGIPAN IN NEXT 41 INCHES. THE SUBSTRATUM IS SILTY CLAY LOAM AND SILT LOAM."|"542041"|"542041:m:458682"
|"Nontechnical description"|"AGR"|"061107"|"Tyler soils make up 80 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is very high.  The depth to a restrictive feature is 15 to 24 inches to fragipan. It is somewhat poorly drained.  The slowest permeability within 60 inches is impermeable.  Available water capacity is moderate and shrink swell potential is moderate.    The top of the seasonal high water table ranges from 6 to 18 inches.  Major component is not a hydric soil.  Land capability class 3w."|"542041"|"542041:m:458683"
|"Nontechnical description"|"AGR"|"061"|"This miscellaneous land type has variable properties that require onsite investigations to determine soil properties and suitability for most all uses."|"542042"|"542042:m:458684"
|"Nontechnical description"|"SO5"|"PA999"|"THESE AREAS ARE MISCELLANEOUS LAND TYPES THAT HAVE NO SOIL OR HIGHLY VARIABLE SOIL PROPERTIES. ONSITE INVESTIGATIONS ARE NEEDED TO DETERMINE THEIR SUITABILITY FOR MOST USES."|"542042"|"542042:m:458685"
|"Nontechnical description"|"SO5"|"PA0140"|"THE VANDERLIP SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH BROWN LOAMY SAND SURFACE LAYER 3 INCHES THICK. FROM 3 TO 21 INCHES IS A YELLOWISH BROWN LOAMY SAND SUBSURFACE LAYER. THE SUBSOIL FROM 21 TO 36 INCHES IS LIGHT YELLOWISH BROWN LOAMY SAND AND FROM 36 TO 68 INCHES IS STRONG BROWN GRAVELLY LOAMY SAND. THE SUBSTRATUM FROM 68 TO 76 INCHES IS YELLOWISH BROWN VERY CHANNERY LOAMY SAND."|"542043"|"542043:m:458686"
|"Nontechnical description"|"AGR"|"061108"|"Vanderlip soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is very low.  It is well drained.  The slowest permeability within 60 inches is rapid.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542043"|"542043:m:458687"
|"Nontechnical description"|"SOI"|"400"|"Extremely stony land consists of steep areas of boulders and rocks on mountain sides. The rocks are mainly quartzite. Tree growth is poor and soils under the stone cover are thin or similar to Laidig or Fleetwood."|"542044"|"542044:m:458691"
|"Nontechnical description"|"AGR"|"061109"|"Vanderlip soils make up 50 percent of the map unit. Areas of rock outcrop make up the remaining portion of the unit. This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  It is well drained.  The slowest permeability within 60 inches is rapid.  Available water capacity is moderate and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 7s."|"542044"|"542044:m:458689"
|"Nontechnical description"|"SO5"|"PA0140"|"THE VANDERLIP SERIES CONSISTS OF DEEP, WELL DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SANDSTONE. TYPICALLY THESE SOILS IN A WOODED AREA HAVE A VERY DARK GRAYISH BROWN LOAMY SAND SURFACE LAYER 3 INCHES THICK. FROM 3 TO 21 INCHES IS A YELLOWISH BROWN LOAMY SAND SUBSURFACE LAYER. THE SUBSOIL FROM 21 TO 36 INCHES IS LIGHT YELLOWISH BROWN LOAMY SAND AND FROM 36 TO 68 INCHES IS STRONG BROWN GRAVELLY LOAMY SAND. THE SUBSTRATUM FROM 68 TO 76 INCHES IS YELLOWISH BROWN VERY CHANNERY LOAMY SAND."|"542044"|"542044:m:458690"
|"Nontechnical description"|"SO5"|"PA0024"|"THE WEIKERT SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN CHANNERY SILT LOAM SURFACE LAYER 7 INCHES THICK. THE SUBSOIL FROM 7 TO 14 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 7 TO 18 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. BEDROCK IS AT 18 INCHES."|"542045"|"542045:m:458693"
|"Nontechnical description"|"AGR"|"061110"|"Weikert soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  This map unit is Farmland of Statewide Importance.  The runoff class is low.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 3e."|"542045"|"542045:m:458692"
|"Nontechnical description"|"AGR"|"061111"|"Weikert soils make up 90 percent of the map unit.  This map unit is in the Northern Appalachian Ridges and Valleys Major Land Resource Area.  The runoff class is low.  The depth to a restrictive feature is 10 to 20 inches to bedrock (paralithic). It is well drained.  The slowest permeability within 60 inches is moderately rapid.  Available water capacity is very low and shrink swell potential is low.   The seasonal high water table is at a depth of more than 6 feet. Major component is not a hydric soil.  Land capability class 4e."|"542046"|"542046:m:458695"
|"Nontechnical description"|"SO5"|"PA0024"|"THE WEIKERT SERIES CONSISTS OF SHALLOW, SOMEWHAT EXCESSIVELY DRAINED SOILS ON UPLANDS. THEY FORMED IN MATERIAL WEATHERED FROM SHALE, SILTSTONE, AND SANDSTONE. TYPICALLY THESE SOILS HAVE A DARK BROWN CHANNERY SILT LOAM SURFACE LAYER 7 INCHES THICK. THE SUBSOIL FROM 7 TO 14 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. THE SUBSTRATUM FROM 7 TO 18 INCHES IS YELLOWISH BROWN VERY CHANNERY SILT LOAM. BEDROCK IS AT 18 INCHES."|"542046"|"542046:m:458694"