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REP15581
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REP15581
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Entry Properties
Last modified
8/24/2016 11:45:05 PM
Creation date
11/27/2007 1:40:35 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977378
IBM Index Class Name
Report
Doc Date
8/10/1982
Doc Name
SANITARY LANDFILL 2 MANAGEMENT AND OPERATION PLAN
From
UTE ENGINEERING AND SURVEYING CO
To
TOWN COUNTRY COORDINATOR
Media Type
D
Archive
No
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The Landfill Operator, under supervision of the Town of SiLverton, <br />' will be required to police the access road and the highway from <br />Silverton to the landfill site. <br />Site Geolo and Soils. The landfill site is located on a:n alluvial <br />' fan at t e southern ase of Storm Peak at elevation 9,440 :Feet. The <br />al uvial fan is of unknown depth but is estimated to be in excess of <br />50 feet. It overlies the Eureka Rhyolite formation which :in turn <br />overlies Precambrian Rock. T e Animas River flows in the •~allev Boor <br />about 30 feet below the e. Refer to e ollo~aing map <br />showing eneral Geology of the area for more details, and to <br />Appendix A for a copy of a Geotechnical Investigation of tailings <br />pond no. 3, the proposed landfill site, prepared by Fox in Rpril, 1976. <br />Test holes in the landfill site in addition to the holes d:cilled by <br />F.px in 1976, were dug with the Town backhoe on July 15, 1982. The <br />holes, a total of four (4), extended to depths of approxim,stely seven <br />(7) feet. The locations of the test holes are shown on the=_ <br />' Togography Map, page 19. Data obtained from the excavation is as <br />follows; <br />' TEST HOLE: 1 2 3 4 <br />ELEVATION 9,442 9,440 9,441 9,441 <br />DEPTH (feet) 7 3 5.5 5.5 <br />SAND (feet) 7 0 0.5 to 3.5 see below <br />' SLIMES (feet) none 1.2 1.5 to 4.5 4.5 <br />NOTES: Test Hole No. 1: Dug to 7 feet. Generally all well drained <br />sa wit small, isolated lenses of clay. Material stable <br />and well drained. Backsloping of 1:1 required for trench <br />excavation. No free water. <br />' Test Hole No. 2: Dug to 2.6 feet. Hole was located on extreme <br />edge of clay surface. Dug through 1.2 feet of slimes and <br />' encountered well drained sand. Correlates well with hole No.l. <br />Test Hole No. 3: Surface was well drained sand. Northern part <br />o t e trenc length of 10 feet, had 6-inches of sand over <br />clay. Southern part of trench had 3.5 feet of san3 over clay. <br />Dug to 5.5 feet, hole kept filling with wet clay, no indication <br />of extent of clay. <br />' Test Hole No. 4: Surface was well drained sand. Excavation <br />s owe foot of sand, 4.5 feet of clay, and sand again. <br />' Unable to excavate deeper. Clay appers limited in extent <br />and could be moved during operation of the landfill. <br />Conclusions from test hole excavation. Considering the location of <br />' clay and sand found in each hole, compared with the assumed cross- <br />sections shown by Fox, we conclude that a section through test holes <br />1 and 2 shows this portion of the pond was constructed using the <br />' downstream method of tailings pond construction. This means that <br />sands will underlie most of the clay material, with the clay <br />increasing in depth toward the decant tube. Test holes 3 and 4 <br /> <br />-13= <br />
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