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2011-08-09_REVISION - M1981185 (60)
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2011-08-09_REVISION - M1981185 (60)
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Last modified
6/15/2021 5:58:15 PM
Creation date
8/10/2011 10:23:22 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1981185
IBM Index Class Name
REVISION
Doc Date
8/9/2011
Doc Name
CN-01 112d permit application Exhibit I thru M
From
Wildcat Mining Corporation
To
DRMS
Type & Sequence
CN1
Email Name
WHE
Media Type
D
Archive
No
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• <br />• <br />Custom Soil Resource Report <br />Interpretive groups <br />Land capability ( nonirrigated): 8s <br />Typical profile <br />0 to 60 inches: Unweathered bedrock <br />251 —Rock outcrop- Snowdon complex, 45 to 75 percent slopes <br />Map Unit Setting <br />Elevation: 8,300 to 11,500 feet <br />Mean annual precipitation: 25 to 40 inches <br />Mean annual air temperature: 30 to 38 degrees F <br />Frost -free period: 40 to 75 days <br />Map Unit Composition <br />Rock outcrop: 60 percent <br />Snowdon and similar soils: 25 percent <br />Description of Rock Outcrop <br />Setting <br />Landform: Mountain slopes, cliffs <br />Landform position (three - dimensional): Mountainflank <br />Down -slope shape: Convex <br />Across -slope shape: Convex <br />Parent material: Volcanic and sedimentary rock and /or granite <br />Properties and qualities <br />Slope: 45 to 75 percent <br />Depth to restrictive feature: 0 inches to lithic bedrock <br />Capacity of the most limiting layer to transmit water (Ksat): Very low to moderately <br />low (0.00 to 0.06 in /hr) <br />Available water capacity: Very low (about 0.0 inches) <br />Interpretive groups <br />Land capability (nonirrigated): 8s <br />Typical profile <br />0 to 60 inches: Unweathered bedrock <br />Description of Snowdon <br />Setting <br />Landform: Mountain slopes <br />Landform position (three- dimensional): Mountainflank <br />Down -slope shape: Linear <br />Across -slope shape: Linear <br />Parent material: Colluvium and residuum derived from rhyolite, sandstone and <br />limestone <br />Properties and qualities <br />Slope: 45 to 75 percent <br />20 <br />
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