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REP35246
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REP35246
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Entry Properties
Last modified
8/25/2016 12:12:26 AM
Creation date
11/27/2007 7:03:54 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1999050
IBM Index Class Name
Report
Doc Name
SLOPE STABILITY ANALYSIS TIMNATH CONNELL PIT
Media Type
D
Archive
No
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4 <br />f <br />/ INTRODUCTTON <br />Connell Resources proposes [o construct a water storage reservoir from a sand and gravel <br />pit known as the Timnath Connell Pit. The Timnath Connell Pit is located in Lazimer <br />County, Colorado at the northeast comer of the intersection of I-25 and County Road 36. <br />The proposed mining operation will extract gravel reserves from the property in some <br />locations that are adjacent to man-made structures. The rules and regulations of the <br />Division of Minerals and Geology require that any mining within a 200 foot setback of a <br />man-made structure show through engineering analysis that the proposed mining will not <br />cause damage. The accepted method of demonstrating this is through a slope stability <br />analysis. This report contains a stability analysis of the mining highwall and the <br />embankment that is proposed for lining the reservoir. The report also provides a general <br />overview of the reservoir, the proposed embankment design, geotechnical results, and <br />methodology, and conclusions and recommendations for construction of the reservoir. <br />OVERVIEW <br />The Division of Minerals and Geology mining plan, exhibit C, proposes that the property <br />be mined in 4 phases. The reclamation plan, Exhibits E and F, proposes future use as a <br />water storage reservoir. Concurrent reclamation is planned in that the reservoir lining <br />will be constructed as the mining progresses. The reservoir will cover an estimated 140 <br />surface acres when full and have a storage capacity of approximately 2000 acre-feet. <br />Actual surface areas and storage capacity will depend on the final configuration of the <br />- reservoir after reclamation is complete. <br />The proposed reservoir will be constructed in the Valley Fill Aquifer. This a shallow <br />` alluvium stratum that varies in thickness up to a depth of approximately 16' for the <br />proposed site. Underlying the alluvium is a relatively impermeable layer of blue/gray <br />siltstone/claystone, called the Pierre Formation. The bore log information (see attached) <br />for this site shows that weathered bedrock (siltstone/claystone) was encountered at depths <br />ranging from 11.5 feet to 15 feet across the site. This will serve as the foundation of the <br />reservoir and will also provide some material for embankment construction. <br />GEOTECHNICAL TESTING <br />In order to evaluate the slope stability of the proposed embankment, geotechnical <br />investigations were performed to obtain the soil types and classifications for the onsite <br />materials. Soil strength properties were estimated based on typical values for similar <br />materials in this region. Table 1 represents a summazy of the results that were used in the <br />stability analysis. <br /> <br />
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