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2008-09-18_REVISION - M1978091UG
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2008-09-18_REVISION - M1978091UG
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Last modified
6/15/2021 5:39:01 PM
Creation date
9/22/2008 4:20:20 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1978091UG
IBM Index Class Name
REVISION
Doc Date
9/18/2008
Doc Name
Response to adequacy review letter
From
Gault Group, INc.
To
DRMS
Type & Sequence
AM3
Email Name
RCO
Media Type
D
Archive
No
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To-date, LKA Int./Richmont Mines Inc. have completed a significant amount of effort to evaluate the <br />hydrologic setting associated with the Level 6 pad. The results of several sampling events remain <br />pending, however it is anticipated that a `Hydrologic Evaluation' document will be provided for BLM, <br />DRMS review in Fall, 2008. Concurrent with the hydrologic evaluation, Black Creek Hydrology <br />associates has obtained 3-dimensional survey points to be able to estimate waste rock volumes, storage <br />capacity volumes etc.. The results of these efforts were incorporated into this reclamation plan. <br />Regardless of the unknown status of the Level 6 pad hydrologic setting, this reclamation plan <br />encompasses a waste rock removal effort which would move waste rock currently residing within the <br />Deadman Gulch natural flow pathway, towards the north (thus occupying a portion of the pad, access <br />road and natural hill slopes). In essence, the material would be rolled-back towards the north to fill in the <br />cut slope created by the pad and road. This approach relies on certain site aspect assumptions as follows; <br />The area to the north of the waste rock pile is largely comprised of alluvium and contains no <br />surface expression of rhyollite (the acid bearing formation associated with Gold Hill) (samples of <br />this material have been collected and analyzed - results were provided in Attachment A, Table <br />A.2). Thus, the placement of the Level 6 waste rock to the north, would put the material on top of <br />a geologic formation found to contain a natural buffering capacity. <br />• It was assumed that there are no groundwater flow pathways that would contact the moved <br />material. This assumption was based upon historic observations which indicate that there are no <br />surface expression seeps along the north side of the exposed portal face, pad or access road. <br />Based on surveyed information, the volume of material to be moved from the estimated native <br />Deadman Gulch channel would range from 9,000 -11,000 cubic yards of material. Very <br />conservative assumptions were folded into this volume estimate (Black-Creek Hydrology <br />sociates Refer to Footnote a below for a description-of how the volume of waste rock was <br />---- --- -- - --- -- <br />tunated using survey information: <br />'guts! B.4 through B.6 depict different facets of the proposed Level 6 pad waste rock removal effort. <br />-- - -- - -- - - <br />I7ie proposed amendment permit boundary as compared to the current permit boundary is shown w'th <br />the gures. The information provided was `estimated' using three-dimensional surveyed points (sh <br />- -- -- <br />Figare B.4 and B.5), gathered?y Black Creek Hydrology -_- LLC in order to determine the volume-of thO <br />- - - <br />waste rock to be removed, and its appropriate placement based on the area it will occupy. Figure B.4 <br />hows the estimated excavation depth to remove the portion of the waste rock pile that occupies the Gulch <br />tive channel. These estimates were based on the hypothesized channel alignment and estimated historic <br />Oontours that were extrapolated from the adjacent exposed ground surfaces (Figure B.6). Figure B.5 <br />demonstrates the conceptual removal effort without layer of information in order to visual the reclamation <br />in absence of features (i.e. structures) that areto be removed as part of reclamation In addition the <br />W?mation obtained from the newly _installed piezometer wells was incorporated as validation porn <br />h were assumptions applied to this estimate as follows:. <br />• Waste rock will be removed 15 feet from the Deadman Gulch flow pathway centerline (narrow <br />blue line `15' Channel offset). The Deadman Gulch flow pathways IS CURRENTLY <br />UNKNOWN, and was estimated using projected underlying topographic contours (wide blue line <br />`Historic Estimated Channel alignment').
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