My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP41946
DRMS
>
Back File Migration
>
Report
>
REP41946
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:43:46 AM
Creation date
11/27/2007 9:09:43 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
4/17/2007
Doc Name
2005 Annual Hydrology Report to Section 8.0
From
Hydro Geo Inc
To
DRMs
Annual Report Year
2005
Permit Index Doc Type
Hydrology 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.
/
51
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
Fina] West Elk Mine 2005 Annual Hydrology Report 16 <br />• 3.2.1.8 Spring 27-1 <br />Spring 27-1 is located in upper Sylvester Gulch (tributary to North Fork) and feeds an area known <br />as "twin ponds". This spring issues from alluvial sediments and is above the south side of mine <br />Panel 15 (Box Canyon mine panel area). Hydrologic monitoring measurements from this station <br />are taken at the end of a plastic drain pipe. <br />3.2.1.9 Sprin¢ G-7 <br />Spring G-7 is located in a western tributary to Sylvester Gulch and is south of the NE mine panel <br />area and north of the SE panel area. This spring issues from joints in a sandstone ledge and has <br />perennial flow, but shows strong seasonal variations with high flows in the spring months. <br />3.2.1.lOSrrinn G-16 <br />Spring G-16 is located in Sylvester Gulch east of the NE mine panel area. This spring issues from <br />a sandstone bed above the F Coal Seam and flows seasonally. It is typically dry in the late summer <br />and fall. <br />3.2.1.11 Spring G-24 <br />• Spring G-24 (decreed spring #8) is located in Sylvester Gulch east of the NE mine panel area. This <br />spring issues from alluvium and is measured at the outflow of a plastic drainage pipe. It flows <br />seasonally and is typically dry in the late summer and fall. <br />3.2.1.12Spring G-14 <br />Spring G-14 (decreed spring #7) is located in Sylvester Gulch east of the NE mine panel area. This <br />spring issues from fractures in the base of a sandstone bed. It flows seasonally and is typically dry <br />in the late summer and fall. <br />3.2.1.13Spring G22 <br />Spring G-22 (decreed spring #3) is located in the Sylvester Gulch drainage on a hillside on the west <br />side of the drainage just south of a mine ventilation shaft and east of the NE mine panel area. It <br />issues from alluvium over a wide area and feeds a wetland on the west side of Sylvester Gulch. <br />Flow diminishes in late summer and autumn. <br />• <br />September 2006 HydroGeo, InC. <br />
The URL can be used to link to this page
Your browser does not support the video tag.