My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
DRMS
>
Day Forward
>
Application Correspondence
>
Coal
>
C2008086
>
2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 3:21:02 PM
Creation date
2/7/2008 3:18:14 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C2008086
IBM Index Class Name
Application Correspondence
Doc Date
1/16/2008
Doc Name
Preliminary Draft Environmental Impact Statement/Subsidence
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.
/
57
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
DRAFT <br />Within the Coal Lease Application area the Cameo Seam outcrop crosses the intermittent <br />stream course in Buniger Canyon approximately 4,500 feet upstream from where it meets the <br />permanent stream in Big Salt Wash. <br />In order to mitigate potential subsidence impacts in the Coal Lease Application area and the <br />immediately adjacent north, east and south parts of the Project Area, it was necessary to have a <br />conceptual mining plan. The goals of the conceptual plan were to maximize safety, then mitigate <br />to the extent possible subsidence impacts and finally to maximize resource recovery. The <br />proposed portal is the anchor for the concept. The conceptual plan that follows involves at least <br />two sets of east-west mains driven off the Big Salt Wash mains. A bleeder entry may well be <br />necessary along the south boundary of the Project Area. Either a bleeder entry or a third set of <br />mains would probably be required along the northern boundary of the Project Area. <br />It will be necessary to drive the main access entries approximately 5,000 feet N 45° E from the <br />planned Red Cliff Mine portal to where it will cross under the overlying intermittent stream <br />course in Stove Canyon at a depth of less than 200 feet., The main entries will probably <br />continue to a distance of approximately 9,000 feet where it will cross beneath the intermittent <br />stream course in Buniger Canyon at a depth of slightly less than 500 feet, still within the Existing <br />Coal Lease area. The N 45° E direction of the Red Cliff Mine main entries indicates that the <br />Main entries will probably turn half-right after passing under Buniger Canyon to drive east just <br />south of the boundary between T. 7 S. and T. 8 S. Driving the .mains in this direction would <br />reach Big Salt Wash in approximately 8,200 feet at a depth of approximately 200 feet. <br />It is anticipated that the main entries will split at Big Salt Wash with one branch continuing to the <br />east, the 1st East Mains, and the other driven to the northeast under Big Salt Wash, the <br />Northeast Mains. The East Mains would be the base for developing longwall panels as much as <br />14,000 feet to the south. If no longwall panels are driven to the north it could be possible to rob <br />the barrier and main entry pillars on the retreat provided the retreat mining was protected by <br />unmined coal on the north side of the 1st East Mains. This assumes that the individual longwall <br />panels driven south off the 2nd East Mains are mined after the 2nd West Mains and that the 2nd <br />East Mains longwall panels are sequenced from east to west and retreated from south to north <br />following the retreat of the 1st East Mains pillars. <br />Retreat mining the 2nd West Mains and the 2nd East Mains would probably require a third set <br />of main entries driven from the East Salt Creek or Munger Creek and across the north end of <br />the Project Area. <br />Mining beneath the permanent and intermittent stream courses will necessitate preventing water <br />loss to the underlying workings. As discussed previously in section 6.1.2 Fractured Zone, water <br />loss to the fracture zone is probable through 100 feet or less of overburden when longwall <br />mining in the Red Cliff Mine Project Area. Big Salt Wash is particularly at risk because it also <br />contains a road and is has agricultural uses. Because there is no available depth of alluvium <br />below any of the deeply incised canyons and the absence of any data on the potential fault <br />control of the nearly trellis drainage pattern in the Project Area, conservatism must be used and <br />a minimum of 200 feet of overburden required to positively prevent water loss from longwall <br />mining under even intermittent stream courses. If ranch animals are pastured at higher <br />elevations in the Project Area, open fractures of more than 2 inches in width could potentially <br />cause injury to range animals, which means 1500 feet of cover potentially could be required in <br />areas with little or no alluvial cover for the planned 11-foot longwall mining height. Table 10. <br />Predicted Surface Fracture Widths Based on York Canyon Mine provides conservative <br />estimates of fracture widths with respect to depth of overburden and panel width. <br />Page 43 of 57 <br />
The URL can be used to link to this page
Your browser does not support the video tag.