My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
1992-06-08_GENERAL DOCUMENTS - C1981017
DRMS
>
Day Forward
>
General Documents
>
Coal
>
C1981017
>
1992-06-08_GENERAL DOCUMENTS - C1981017
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/22/2021 7:38:53 AM
Creation date
10/3/2012 10:40:32 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981017
IBM Index Class Name
GENERAL DOCUMENTS
Doc Date
6/8/1992
Doc Name
Bid Documents (IMP)
Permit Index Doc Type
General Correspondence
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.
/
86
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
Underground workings extend from the portal areas, which are in <br /> Coal Basin, beneath Huntsman Ridge, and underlie the west and south <br /> slopes beyond Huntsman Ridge. Huntsman Ridge is the dividing line <br /> between Pitkin and Gunnison Counties, and the White River and <br /> Gunnison National Forests. <br /> Geology <br /> The structure of the Coal Basin is thought to have been formed <br /> by the doming of sedimentary strata over an igneous intrusion. <br /> Faulting is common, and is a significant determinant of the <br /> drainage pattern in Coal Basin, having directly or indirectly <br /> controlled Bear Creek, all forks of Dutch Creek, both forks of <br /> Oilwell Creek, Porcupine Creek and Coal Creek. <br /> Topography <br /> Coal Basin is characterized by steep, erratic, deeply eroded <br /> terrain. Elevations range from 7,180' at the confluence of <br /> Coal Creek with the Crystal River, to 8,000 at the central <br /> complex yard area, to 11,8501 along Huntsman Ridge. Areas of <br /> moderate terrain are rare. <br /> The erosion cycle of Coal Basin is estimated at 36,000,000 <br /> years, to the Eocene era. The outcropping strata in Coal <br /> Basin are, for the most part, highly erosive, particularly the <br /> Mancos Shale, which floors most of the basin and is the most <br /> common unit. As a result, Coal Basin is characterized by a <br /> highly eroded topography. <br /> Drainage <br /> The primary stream in Coal Basin is Coal Creek, a perennial <br /> stream, tributary to the Crystal River. This stream drains an <br /> area of 26 square miles. Streams and stream segments <br /> tributary to Coal Creek include Bear Creek, the South Fork of <br /> Dutch Creek, the North Fork of Dutch Creek, Oilwell Creek, <br /> Porcupine Creek, Spring Creek and Braderich Creek. Mine <br /> facilities are situated in the drainages of Coal Creek, North <br /> and South Dutch Creek. <br /> climatic Conditions <br /> Precipitation averages approximately 29 inches per year, of <br /> which 70% falls in the form of snow. Snowfall begins in <br /> October, and snowpack continues through May. <br /> Surface Use In Addition to Mining <br /> Livestock have grazed Coal Basin since 1946, under permit from <br /> the U.S. Forest Service, and the use continues during the <br /> summer months. <br /> VI. MINING OPERATIONS AT THE SITE <br /> A. Historic Use <br /> Crystal Springs Coal, Inc. 9 Coal Basin Mine <br />
The URL can be used to link to this page
Your browser does not support the video tag.