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PERMFILE47848
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PERMFILE47848
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Entry Properties
Last modified
8/24/2016 10:49:51 PM
Creation date
11/20/2007 1:19:20 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977211
IBM Index Class Name
Permit File
Doc Date
3/14/1980
Doc Name
RESTATED APPLICATION FOR MINING AND RECLAMATION PERMIT
Media Type
D
Archive
No
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<br /> <br />that is why we included the words "or some other use." The stockpond <br />• is there as an accomodation to a previous landowner for his cattle. <br />9) P-E-B - Please describe in greater detail why it is not <br />felt that there will be slippage or movement of the plant medium. <br />The S.C.S. report states that this material has a moderate to high <br />erosion hazard. <br />RESPONSE D9. As far as we can determine the S.C.S. report <br />is referring to the native soil (the Paunsaugunt Series) and not this <br />medium. Furthermore, the high erodibility of the Paunsaugunt Series <br />is not borne out by observations. In fact it appears to be less <br />erodable than the Kutler-Broadmoor Complex. Experience in the <br />past, even with steep slopes (2:1 and more) at both Pikeview and <br />Queen's Canyon, has shown very little erosion of the material and <br />• slippage is quite rare except on slopes in excess of 45°_ where, on <br /> occasion slippage has occurred when downslope support has been <br />removed. <br />Slumps, mudslides, landslides, and creep are all heavily <br />related to an instability of the material when moisture levels increase <br />beyond the capability of the slope and the substrate to hold them. <br />Solifluction in arctic soils can occur on 15:1 slopes because the soil <br />is saturated with tons of water and the mass is resting on a very <br />smooth, highly lubricated clay surface that is about as slippery <br />as greased glass. <br />The substrate here is a rough surface of rock that is <br />partially fractured. The material itself has a very high <br />permeability and retains very little water to increase mass to such a <br />u <br />P-E-16* <br />
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