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2016-12-19_REVISION - M1980244 (2)
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2016-12-19_REVISION - M1980244 (2)
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Last modified
12/22/2016 11:28:00 AM
Creation date
12/22/2016 11:12:37 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
Revision
Doc Date
12/19/2016
Doc Name
Responses to DRMS ECOSA Stability Review Comments
From
Newmont / CC&V
To
DRMS
Type & Sequence
AM11
Email Name
TC1
AME
ERR
Media Type
D
Archive
No
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Technical Memorandum <br />Newmont CC&V Gold Mine <br />East Cresson Overburden Storage Area Stability Review/Update <br />NewFields Job No. 475.0106.005 <br />9 December 2016 <br /> <br /> <br />Page 5 <br /> Overburden: Overburden material in the ECOSA is essentially rockfill from the pits with no <br />economic value. As such, the engineering properties are similar to that of the ore that has <br />been studied throughout the project history and modeled with a 39 or 40 degree friction <br />angle. In agreement with older designs, the initial evaluation of the ECOSA considered a <br />friction angle of 39 degrees (Adrian Brown, 2012). Based on the project history and new <br />laboratory test data (measured friction angle of 41 degrees), the continued use of a 39 <br />degree friction angle to represent the strength of the overburden was deemed reasonable <br />and applied in the current evaluation. <br /> Colluvium: Strength parameters for the colluvium foundation was based on the recent <br />laboratory test data and existing data from around the site for unconsolidated foundation <br />materials. Adrian Brown (2012) characterized the strength of the colluvium under the <br />ECOSA using an empirical relationship between shear strength, liquid limit and clay fraction <br />of the material. Based on visual observation of colluvium and recent test data, this value is <br />too conservative for a coarse‐gravel with minimal fines. The current evaluation uses an <br />average value between the recent laboratory data and that utilized by Adrian Brown (35 <br />degree and no cohesion). As some of the fines within the colluvium are fine‐grained, the <br />strength was reduced by 20 percent for the pseudostatic evaluation to account for <br />development of excess pore pressure. <br /> Bedrock: The dominant rock type underlying the facility is Tertiary phonolites. The unit <br />weight and strength for bedrock was developed from data presented by Call & Nicholas <br />(2015) for this material type and a poor to fair rock quality designation (40 – 60%). The <br />associated unit weight, φ and cohesion values are 153 pcf, 34.5 degrees and 20,000 psf, <br />respectively. <br /> Stability Evaluation Results 3.4 <br />The stability analyses resulted in acceptable minimum FOS values for both static and pseudo‐ <br />static conditions, as show in Table 2.2. The output graphics from the stability models are <br />included as Attachment C. <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />
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