My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE108426
DRMS
>
Back File Migration
>
Permit File
>
100000
>
PERMFILE108426
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:00:54 PM
Creation date
11/24/2007 4:49:02 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Permit File
Doc Date
5/13/2002
Doc Name
Geotechnical Investigation Deserado Coal Mine Waste Banks
Section_Exhibit Name
Illustration 21
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.
/
70
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
-3- <br />protected by a trash mntrol rack, and the outlet pipe will be <br />• provided with seepage cellars. <br />The emergency spillways for the sedimentation pond will be lined <br />with riprap to reduce erosion in the invert of the spillway channel. <br />If loadings or conditions are significantly different from those <br />described above, we should be notified to re-evaluate the reco~mnenda- <br />tions contained in this report. <br />GDOlAGIC SETPING <br />The proposed Deserado Mine refuse disposal site is located in <br />the northwestern part of the Pieeanoe structural basin about 15 miles <br />northeast of Rangely, ~lorado. The site will be situated along a <br />small, east-trending tributary to Red Wash. The disposal site is <br />• about 3 miles northeast of the mine portal as shown on Fig. 2. The <br />disposal site is located near the northwest trending axis of the Red <br />Wash syncline which is an asymmetric, secondary fold along the <br />northern part of the Piceanoe structural basin. The axis of the <br />syncline is shown on Fig. 3. Bedroc3c of the Upper Cretaceous age <br />- Mesaverde Formation underlies the surficial deposits at the site. The <br />Mesaverde is underlain bf Mesozoic to Precambrian age sedimentary <br />rocks which extend to depths of several thousand of feet. Major <br />faults have not been mapped in the vicinity of the site, Id~wley and <br />others (1979). Tne closest faults which have been designated possible <br />capable faults are located in the Rangely Oil Field about 9 miles <br />southwest of the site and along the northern and southern margins of <br />the Uinta Atd~ about 17 to 50 miles north of the site, Kirkham and <br />• Rogers (1978). <br />
The URL can be used to link to this page
Your browser does not support the video tag.