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GENERAL34948
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GENERAL34948
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Last modified
8/24/2016 7:56:10 PM
Creation date
11/23/2007 8:07:05 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982057
IBM Index Class Name
General Documents
Doc Date
11/23/1993
Doc Name
MEMO C-82-057 SENECA IIW PIT ADVANCEMENT STABILITY CONCERNS
From
DMG
To
SUSAN BURGMAIER
Permit Index Doc Type
GENERAL CORRESPONDENCE
Media Type
D
Archive
No
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III IIIIIIIIIIIIIIII <br />999 <br />DIVISION OF MINERALS AND GEOLOGY <br />Department o(Nalural Resources <br />1313 Sherman SI., Room 215 <br />Denver, CO 80203 <br />Phone: (303) 8663567 <br />fAX: 13031832-8106 <br />STATE OF COLORADO <br />To: Susan Burgmaier, Environmental Protection Specialist <br />From: Bruce Stover, Technical Support <br />Date: November 23, 1993 <br />Re: C-82-057 Seneca IIW Pit Advancement Stability Concerns <br />OF ~~ <br />R'" 4 <br />Nei <br />/ ~~ <br />• ~~• <br />• ~ r8i6 <br />Roy Romer <br />Governor <br />Michael B. Long <br />Division Dnecmr <br />I have reviewed the photographs and materials you gave me pertaining to our discussion of <br />the stability concerns on the north side of the Seneca IIW pit wall near the recent landslide. <br />The photographs and drill log clearly suggest a potential for surface movement and <br />disruption beyond the edge of the pit as it is advanced northwards, east of the recent <br />landslide. <br />The photographs show that the brown overburden materials exposed in the pit wall at the <br />recent slide were moving downslope toward and into the pit, due in part to removal of down <br />slope support by the pit excavation. There is reason for similar concern that this same <br />mechanism could create slope instability farther east of the recent event. Northward <br />advancement of the pit in that location may result in eventual loss of support for <br />approximately 47 feet of 'brown", presumably overburden materials, consisting of old <br />landslide deposits and weathered shale above bedrock. If this slope fails in similar fashion <br />to the recent event, propagation of surface movement and disruption could potentially <br />progress far enough upslope above the pit to adversely affect the topsoil stockpile near the <br />top of the slope. <br />If the pit is to be advanced farther northwards, I suggest that two or three inclinometers, (or, <br />alternatively, a time-domain-reflectometer {TDR} set up), be installed into the <br />overburden/bedrock contact between the pit wall and the topsoil stock pile to monitor any <br />movement which could occur. If checked every few days, these devices should be able to <br />detect slope creep and slope movement incipient to a major slope failure event prior to <br />initiation, allowing appropriate action to prevent damage to the topsoil pile and undisturbed <br />areas beyond the limits of the pit. In lieu of this approach, or of a slope stability analysis <br />specific to this concern, it's a gamble on whether or not a serious slope instability problem <br />would occur which could cause adverse effects for adjacent areas and facilities. When <br />mining in landslide-prone terrain, these situations can be expected to occur. <br />
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