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2024-03-04_REVISION - M1995095
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2024-03-04_REVISION - M1995095
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Entry Properties
Last modified
3/5/2024 8:20:23 AM
Creation date
3/5/2024 8:07:41 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1995095
IBM Index Class Name
Revision
Doc Date
3/4/2024
Doc Name
Request For Conversion
From
Hill Top Gravel, LLC
To
DRMS
Type & Sequence
CN1
Email Name
HR1
EL1
Media Type
D
Archive
No
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Custom Soil Resource Report <br /> Minor Components <br /> Truckton <br /> Percent of map unit: 10 percent <br /> Landform: Interfiuves <br /> Landform position(two-dimensional):Summit <br /> Landform position(three-dimensional): Interfluve <br /> Down-slope shape: Linear <br /> Across-slope shape: Linear <br /> Ecological site: R049XB21000-Sandy Foothill <br /> Hydric soil rating: No <br /> Yoder <br /> Percent of map unit: 5 percent <br /> Landform:Alluvial fans <br /> Down-slope shape: Linear <br /> Across-slope shape: Linear <br /> Ecological site: R049XY214C0-Gravelly Foothill <br /> Hydric soil rating: No <br /> 22—Cushman loam, 1 to 5 percent slopes <br /> Map Unit Setting <br /> National map unit symbol: 367t <br /> Elevation: 6,000 to 6,500 feet <br /> Mean annual precipitation: 14 to 16 inches <br /> Mean annual air temperature: 46 to 50 degrees F <br /> FroFt-free period: 125 to 145 days <br /> "` Farmland fofprirtiefai•mlaria'' - <br /> Map Unit Composition <br /> Cushman and similar soils:98 percent <br /> Minor components:2 percent <br /> Estimates are based on observations, descriptions, and transects of the mapunit. <br /> Description of Cushman <br /> Setting <br /> Landform: Hills, flats <br /> Landform position (three-dimensional): Side slope,talf <br /> Down-slope shape: Linear <br /> Across-slope shape: Linear <br /> Parent material: Residuum weathered from sandstone and shale <br /> Typical profile <br /> A -0 to 5 inches: loam <br /> Bt-5 to 17 inches: sandy clay loam <br /> Bk- 17 to 23 inches: sandy clay loam <br /> Ck-23 to 30 inches: fine sandy loam <br /> Cr-30 to 34 inches: weathered bedrock <br /> 14 <br />
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