My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE70512
DRMS
>
Back File Migration
>
Permit File
>
800000
>
PERMFILE70512
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 11:19:44 PM
Creation date
11/20/2007 11:23:46 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981014
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
MR-14 to MR-20
Section_Exhibit Name
EXHIBIT 15 Part 3
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.
/
36
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
Southficld Minc <br />Minor ReHSion Request Na. 10 -South Fan Installation • S <br />Cultural and Historic Resources (2.04.4) <br />The Monarch No. 4 Mine is identified as a possible historical site evaluated <br />by the Colorado Historical Society in Exhibit 6, Cultural and Historic <br />Resource Information, of the EFCI permit document. This documentation <br />indicates that the evaluation resulted in a determination that the site is not <br />eligible for listing. Also refer to Section 2.04.3 of the EFCI permit <br />application document (Volume 11. <br />Geology (2.04.6) <br />Geology of the area to be effected by the proposed fan installation is <br />consistent with surrounding areas within the EFCI permit area. Surficial <br />• materials consist of geologically recent interbedded outwash deposits of <br />soil, sand, silt and conglomerates. The site is located near the base of a <br />small intermittent drainage which has cut through the outwash materials <br />exposing the Vermejo formation on the valley sides. The existing mine <br />portals are in the Red Arrow coal seam. The Red Arrow seam is part of the <br />Vermejo formation which consists predominantly of sandstones and fine- <br />grained siltstones. <br />The dominant structural features in this area are the Wet Mountain Fault <br />and adjacent Chandler Syncline. The synclinal axis is located approximately <br />3,000 feet southwest of the proposed site and the fault is an additional <br />4,500 feet to the southwest. This is no history or evidence of any <br />geologically recent movement along the fault. <br />While some surficial sloughing of exposed material from the existing portal <br />• bench has occurred, there is no evidence of any significant rock mass <br />failure. In addition, the portal bench is cut into the existing valley side <br />which slopes at <br />AQ Int. • P.O. Bar 774018• SYtanbaol Spnngr. Colorado 80177• (303)876360 <br />
The URL can be used to link to this page
Your browser does not support the video tag.