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PERMFILE136072
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PERMFILE136072
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Entry Properties
Last modified
8/24/2016 10:36:46 PM
Creation date
11/26/2007 4:10:47 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2006010
IBM Index Class Name
Permit File
Doc Date
1/24/2006
Doc Name
110c Appl
From
MS Forest LLC
To
DMG
Media Type
D
Archive
No
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SITE DESCRIPTION <br />SOILS INFORMATION <br />EXHIBIT B <br />The following information was obtained from site observa- <br />tions and the basic soils and vegetation information found on <br />line thru the USDA's National Soils information pages. The <br />following soils information is made part of this application. <br />Soil units are shown on the USDA map, reproduced on page 7 <br />following this text. The photo map shows the surrounding vegeta- <br />tion features and soil types. This site lies along the southern <br />edge of a ridgline between Jarosa Canyon on the north and an <br />unnamed draw on the south. <br />This deposit is an deep gravelly deposit underlaying the <br />Davtone loam, 5 to 20% slopes soil series . The general soils description <br />that follows indicates that this soil is fairly deep. However, <br />on this site we found that the dark usable topsoil varies from 10 <br />to 12 inches. Underlaying this topsoil is a red clay sandy loam <br />with gravel intermixed that will provide binder for the roadbase <br />material we plan to produce. The description is consistent with <br />that described in the USDA text. The gravel depth on the site <br />appears to be as deep as 100 plus feet since it is visible from <br />the top of the ridgline to the base of the road that runs along <br />the south side of the permit area. Along the edges of the <br />hillside along the road the gravel is visible and the land owner <br />reports that this visible gravel extends into the hillside and is <br />not a shallow cover that has sloughed off the top and trickled <br />down the sides. On this site the ridgline between a creek on the <br />north and the canyon along the south appears to be an alluvial or <br />colluvial fan resulting from glacial till left as the glaciers <br />retreated to the west. <br />4 <br />
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