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REP28368
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REP28368
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Entry Properties
Last modified
8/24/2016 11:59:02 PM
Creation date
11/27/2007 5:02:50 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977300
IBM Index Class Name
Report
Doc Date
2/1/1983
Doc Name
SCHWARTZWALDER MINE WASTE ROCK PILE STABILITY
Media Type
D
Archive
No
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<br />• and mine waste dumps have been further identified in the area. <br />Surface geologic mapping, supported by an evaluation of aerial <br />photographs available for the site, was performed so that individual <br />geotechnical units could be delineated and characterized for t:he purpose <br />of this study. The geotechnical mapping performed within thi<, study was <br />also used to provide data on the general stability of the area. <br />The results of geotechnical mapping are shown on Plzite 2, feo- <br />technical Map. In this map, the area of interest was divided into several <br />geotechnical units that are important for the scope of work. Following <br />is a brief description of these geotechnical units: <br />Man-made fills cover a considerable area on the southern part <br />of the property where most of the mine surface facilities ar•e located. <br />They appear to be spread over most of the alluvial valley of Ralston <br />Creek; minor fills have been constructed along the road on tY~e northern <br />• end of the property. Fills consist predominantly of cobbles and gravels. <br />Waste piles are located in the northern part of thE~ property, <br />on both sides of Ralston Creek. For the purpose of this report, they <br />are called East and West piles. <br />Alluvial sediments of Ralston Creek occur along the creek <br />within the entire area covered by this study. The width of alluvial <br />deposits is limited on the northern end of the property anc increases <br />toward the south. The maximum width of the alluvial sediments is ap- <br />parently at the location of the mine and other surface facilities, <br />although the alluvium is obstructed by the cover of the man-Wade fills. <br />Alluvial sediments are also covered by both waste piles; an attempt <br />was made to indicate the original alluvial boundaries on the geotechni- <br />cal map. The alluvial deposits consist predominantly of cobbles and <br />gravels with some sand. The color of the sediments is medium brown. <br />Alluvial soils are frequently well-sorted, forming lenses of similar <br />L <br />- ~ - <br />
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