My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP43696
DRMS
>
Back File Migration
>
Report
>
REP43696
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:45:58 AM
Creation date
11/27/2007 9:58:50 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
1/9/2003
Doc Name
Subsidence Field Observations August 27-29, 2002
From
Mountain Coal Company
To
DMG
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.
/
26
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
' Subsidence Field Observations <br />West Elk Mine <br />August27-29,2002 <br />' <br />' 2.0 FIELD DIFFERENTIATION OF CRACKS IN MINING AREAS <br />' 2.1 Subsidence Cracks <br />Subsidence cracks are open cracks that occur in the zone of maximum tension above a mining <br />panel where the ground undergoes extension. This zone of maximum tension occurs <br />approximately transverse and longitudinal to the orientation of the longwall mining panel. Crack <br />orientation can be variable, as with other deformational processes in nature. Transverse and <br />longitudinal subsidence cracks often do not conform to a precise pattern as discussed above. <br />Joints in the overburden rocks, for example, may influence the orientation of both the transverse <br />and longitudinal tension cracks. <br />Transverse cracks occur above the longwall mining faces-these cracks aze located roughly <br />transverse to the long axis of the panel-thus the name transverse tension cracks. Transverse <br />cracks normally have a very dynamic history. These cracks open when the longwall face moves <br />beneath the azea of observation, then often close again when the longwall face moves out of the <br />area of its mining influence. <br />Longitudinal cracks occur along the edges of the longwall mining panel-these cracks aze <br />oriented roughly pazallel to the long axis of the mining panel-thus the name longitudinal <br />tension cracks. The longitudinal tension cracks normally remain open, because the overburden <br />permanently moves downward into the mined-out panel. <br />Pseudo subsidence cracks aze quite common on ridges and near cliffs. These cracks can look <br />very much like subsidence cracks. The extensive crack along a narrow ridge on West Flatiron is <br />a good example of a pseudo subsidence crack. In this case it was easy to determine that the crack <br />was not mine related, because no mining has occurred in the azea. The presence of pseudo <br />subsidence cracks is a good reason to do baseline studies prior to mining so that these features <br />can be recorded prior to mining. <br />831-032.570 Wright Water Engineers, Inc. Page 3 <br />December 2002 <br />
The URL can be used to link to this page
Your browser does not support the video tag.