My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP23356
DRMS
>
Back File Migration
>
Report
>
REP23356
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 11:55:47 PM
Creation date
11/27/2007 3:41:03 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
1/30/2007
Doc Name
2006 Subsidence & Geologic Field Observation
From
Mountain Coal Company, LLC
To
DRMS
Permit Index Doc Type
Subsidence Report
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.
/
48
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
2006 Subsidence and Geologic Field Observations <br />Box Canyon, West Flatiron, Apache Rocks, and South of Divide Mining Areas <br />influence. Crack duration, in areas of permanent tension-such as above solid coal boundaries <br />or rigid chain pillazs, is summarized (from eazlier annual observation reports) as follows: <br />1. Cracks in colluvium commonly heal and re-vegetate in about one to three years. <br />2. Cracks in soft, friable bedrock, such as the soft sandstone above mined longwall panel 13 <br />(Apache Rocks Mining azea), are no longer visible in roughly three to six years. <br />3. Cracks in hard, durable bedrock, such as the sandstone outcrop at Apache Rocks, will <br />likely be visible for many decades. <br />No mining effects on rockfalls or landslides were observed in the Apache Rocks mining area. <br />However, fresh-looking cracks and scarps have been recently observed, suggesting that local, <br />sporadic falls and slides continue in the rockfall/landslide area near the head scarp of the first <br />east drainage of Sylvester Gulch. Rockfalls and landslides in this area located above mined <br />longwall panel 22, are categorized as having a very high rockfall potential. Rockfall and <br />landslide activity was notably accelerated during the mining of longwall pane122. <br />Field observations, and a review of aerial photographs, indicate the excavation azea for the Deer <br />Creek ventilation shaft and escapeway for the South of Divide mining area is at least partially <br />constructed in the lower part (toe area) of a landslide slump block (Maps 1 and 2). Lateral <br />support of the slump block in the western part of the excavation area has subsequently been <br />reduced. Although the landslide appears to have been stable over the last 43 years, based on the <br />U.S. Geological Survey (USGS) aerial photos dated 1963, continued stability will likely depend <br />on adequate dewatering of the landslide material in the excavation azea. <br />It is the author's opinion that annual field observations are adequate to evaluate the effects of <br />longwall mining in the West Elk Mine area. This opinion is based on the following: <br />1. The duration of subsidence effects is considerably longer than one yeaz. <br />831-032.750 Wright Water Engineers, Inc. Page 2 <br />December 2006 <br />
The URL can be used to link to this page
Your browser does not support the video tag.