My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2012-02-28_REVISION - M1980244 (95)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1980244
>
2012-02-28_REVISION - M1980244 (95)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 4:49:13 PM
Creation date
3/9/2012 12:17:39 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
REVISION
Doc Date
2/28/2012
Doc Name
VOL. 2, Appendix 2: Hydrologic Evaluation Part 1
From
CRIPPLE CREEK & VICTOR GOLD MINING COMPANY
To
DRMS
Type & Sequence
AM10
Email Name
TC1
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
104
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
1.0 INTRODUCTION <br />Cripple Creek & Victor Gold Mining Company (CC &V) operates the Cresson Project, a gold <br />mining and processing operation in the Cripple Creek Mining District ( "District "). The Cresson <br />Project is located between the cities of Cripple Creek and Victor, Colorado southwest of Pikes <br />Peak. <br />The gold mineralization in the District occurs primarily in the Cripple Creek Diatreme — an <br />alkaline volcanic diatreme - intrusive complex ( "Diatreme "). The country rocks surrounding the <br />Diatreme are dominantly Precambrian in age and include gneiss, schist, quartz monzonite, augen, <br />gneiss /granodiorite and granite. The Diatreme is a steep - walled crater with a crudely elliptical <br />outline at the surface. The volcanic activity which created the Diatreme took place during the <br />Tertiary period, approximately 32 million years ago and included placement of plugs, flow <br />domes, small stocks and late -stage diatremal pipes and dikes. Following the placement of the <br />diatreme rock, the rocks were subjected to intense potassium metasomatism, hydrothermal <br />brecciation and gold mineralization. Carbonate -rich styles of alteration post date the precious <br />metal mineralization event. The carbonate alteration plays a major role in the ground water <br />chemistry of the area, as evidenced by the alkaline nature of regional ground water draining from <br />the Carlton Tunnel <br />The District has been historically mined for over 100 years. In order to effectively mine at <br />deeper depths, as the District was developed a series of progressively deeper drainage tunnels <br />were constructed to drain the ground water. The deepest tunnel, the Carlton Tunnel, was <br />completed in 1941 and has dewatered the rock in the District to an elevation below <br />approximately 7,000 feet. <br />This report presents a brief description of the surface water flows and drainage basins in the <br />vicinity of the Cresson Project and a compilation of the surface water and ground water <br />monitoring data for active monitoring locations. The report also discusses currently approved <br />activities and planned activities under the Cresson Project Mine Life Extension 2 ( "MLE2 ") and <br />potential effects to surface and ground water as a result of those activities. A separate report <br />titled "Cresson Project Hydrogeochemical Evaluation" dated February 2012 and prepared by <br />Adrian Brown Consultants, Inc. ( "ABC ") has also been prepared for MLE2. That report <br />addresses the hydrogeological and geochemical properties associated with MLE2. Certain <br />discussions contained in this report rely on the ABC report and contain references to data in the <br />ABC report. <br />'Cripple Creek & Victor Gold Mining Company <br />Cresson Project Hydrologic Evaluation for Mine Life Extension 2 <br />1 <br />
The URL can be used to link to this page
Your browser does not support the video tag.