My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
1995-08-11_REVISION - M1977493 (10)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1977493
>
1995-08-11_REVISION - M1977493 (10)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/16/2021 6:27:01 PM
Creation date
9/14/2010 12:30:24 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977493
IBM Index Class Name
REVISION
Doc Date
8/11/1995
Doc Name
EPP-III
From
CMC
To
DMG
Type & Sequence
TR7
Email Name
ACS
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
82
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
01/11/1995 08:36 2168648136 MVTECHNOLOGIES, INC. PAGE 05 <br /> 2 P1 LX= CATION <br /> Statement of Problem <br /> The major problem at the McNulty rock dump is the acidification of surface <br /> water and groundwater by contact with acid-generating waste rock. The acid <br /> mine drainage (AMD) emerges at the toe of the waste rock dump and is collected <br /> in a holding pn*ic1. <br /> Site Description <br /> The McNulty waste rock dump is a part of the Climax Molybdenum Company mine <br /> located in Climax, Colorado. The dump covers approximately 450 acres. <br /> Overburden rock from the operation of the surface pit is transported by truck <br /> to the dump and is end dumped. Bulldozers then place and compact the rock. <br /> The dump has been constructed in a series of benches with relatively steep <br /> outslopes ranging from 1.5:1 to 2:1. <br /> There are approximately five distinct rock types in the dump. The molybdenite <br /> occurs disseminated in quartz veins transversing granite. Upon oxidation, the <br /> material acquires an orange-red cast indicating that ferric oxides <br /> predominate. <br /> The rock deposited at the dump ranges in size from large boulders to fines. As <br /> a result the majority of the large rock is found at the base of each lift and <br /> this creates large void areas within the dump for the passage of infiltrating <br /> ground and surface water. There are no surface water diversion channels to <br /> keep the water from contacting the waste rock. All precipitation and snowmelt <br /> from the upgradient watershed passes over and through the- rock dump. <br /> There are some perched water tables that discharge groundwater into the dump. <br /> All of the infiltrating ground and surface water eventually emerges as AMD at <br /> the toe of the waste rock dump. This AMID is collected in a holding pond where <br /> it is allowed to evaporate. If the pond should overflow, the water can either <br /> be diverted to the water processing system or to the Robinson tailings pond. <br /> The McNulty rock dump is still available for further rock disposal when the <br /> Climax Mine is reactivated. Presently, the mine is inactive due to economic <br /> conditions. <br /> Site Visit and Sampling <br /> Water samples (Table 1) , waste rock samples (Table 2), and photographic <br /> records of the site were obtained. A visual inspection of the site was <br /> conducted. <br /> Semple Preparation and Laboratory Analyses. All waste rock samples were air- <br /> dried, mixed., pulverized and riffle split into representative subsomples for <br /> chemical analysis. <br />
The URL can be used to link to this page
Your browser does not support the video tag.