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PERMFILE108501
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PERMFILE108501
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Last modified
8/24/2016 10:00:58 PM
Creation date
11/24/2007 4:57:15 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
April 1981 Report
Section_Exhibit Name
Exhibit 14 Landslide Study
Media Type
D
Archive
No
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I. The site lies along the westerly flank of the West Ells Mountains within the drainage <br />basin of the North Fork of the Gunnison River. Both Sylvester Gulch, to the east, <br />and "No Name" Gulch, to the west of the plant site, drain into the river. The <br />average annual precipitation is ten inches along the river. Most o! the precipita- <br />tion falls as snow during the winter months, while the sparse summer precipitation <br />consists of isolated thunderstorms. Temperatures range from 30°P in the winter to <br />90°F± in the summer, with the mean temperature about 70°F. Depth of surface <br />freezing is approximately 54 inches. The plant site is densely covered with tall <br />grasses and shrubs, consisting primarily of Gambol oak and Saskatoon serviceberry. <br />B. Soils Investigations: <br />An extensive subsurface soils investigation was performed by Chen and Associates <br />during the early summer oP 1980. This investigation included the drilling of <br />approximately fifty (50) exploratory test holes and the setting of approximately <br />sixteen (16) piezometers. Tests were performed to determine shear strength, <br />bearing capacity, permeability, compaction, compressibility and swelling <br />characteristics of the various materials. Chen and Associates submitted a report <br />on both the initial investigation and a subsequent boring program. Refer to <br />Geotechnical Site Evaluation, Job No. 20,240, dated July Sl, 1980. <br />C. Landslide Investigations: <br />A geotechnical investigation into possible landslide areas at the site was conducted <br />by Geo-Hydro, Ina, during the Summer of 1980. Their findings indicate that the <br />~~ prime area for potential landslides is in the area above the natural bench at <br />~,,,~ elevation 6,400 plus or minus. Their investigation was centered primarily on the <br />requirements for construction of the Portal Bench, Access Road, Substation pad, <br />and shop warehouse pad. It was their conclusion that the stability of any cuts <br />within the landslide boundary is directly related to the saturation state in the upper <br />fifteen (15) feet of the soils. As such, a dewatering system was designed and will <br />be constructed to lower the water levels and, thus, stabilize the existing ground and <br />the planned construction within these areas. <br />The landslide report did not address the reclamation procedures to be followed for <br />the facilities within the landslide boundary. However, information contained in <br />that report was utilized for the investigations included in the report herein. <br />D. Piezometer Monitoring Program: <br />The ARCO Coal Company has contracted with the WATEC Company to perform <br />periodic measurements on the piezometers installed by Chen and Associates. The <br />WATEC Company will be continuing their monitoring operations throughout the <br />construction of the ML Gunnison Project to ensure that the dewatering system is <br />operating properly. Such monitoring should be continued throughout the <br />operational life of the mine. <br />l~ <br />
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