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2012-07-02_REPORT - C1980007 (3)
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2012-07-02_REPORT - C1980007 (3)
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Last modified
8/24/2016 5:02:08 PM
Creation date
7/3/2012 11:19:12 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Report
Doc Date
7/2/2012
Doc Name
2011 Annual Hydrology Report
From
HydroGeo Inc
To
DRMS
Annual Report Year
2011
Permit Index Doc Type
Hydrology Report
Email Name
JRS
DIH
Media Type
D
Archive
No
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West Elk Mine 2011 Annual Hydrology Report 30 <br />3.2.1.14 Deep Creek Trail Spring <br />Deep Creek Trail Spring is located in upper Deep Creek which is tributary to the <br />North Fork of the Gunnison (Map 2). This spring is located in the SOD mine plan area. <br />The source of this spring appears to issue from alluvium. Baseline monthly monitoring <br />of the Deep Creek Trail Spring began in the spring of 2007 and included measuring flow, <br />collecting field water quality data, and collecting samples for laboratory water quality <br />analyses from May through October 2007 (CDRMS, 2006). Routine monitoring (3 times <br />per year) at this location commenced in WY 2008. <br />3.2.2 Springs above the B -Seam in the Box Canyon Area in the <br />North Fork Drainage Basin <br />3.2.2.1 Spring 11 -2 <br />Spring 11 -2 is located east of Box Canyon on a hillside on the south side of the <br />North Fork of the Gunnison (Map 2). This spring is situated north of the Box Canyon B- <br />seam panels. It issues from alluvium below a sandstone cliff, has seasonal flow, and is <br />often dry in summer and autumn. Monitoring at this spring began in 2000. <br />3.2.2.2 Spring 10 -1 <br />Spring 10 -1 is located on the east side of Lower Box Canyon (Map 2). It is <br />situated north of the Box Canyon B -seam panels and issues from alluvium on slopes <br />tributary to the North Fork. Flow is variable and does not follow a seasonal pattern. <br />Monitoring at this spring began in 1999. <br />3.2.2.3 Spring E10 -2 <br />Spring E l 0 -2 is located on a hillside east of an unnamed drainage tributary to the <br />North Fork between Sylvester Gulch and Box Canyon (Map 2). This spring is situated in <br />landslide material below a fractured sandstone cliff north of the Box Canyon B -seam <br />panels. Low flows were observed in WY 2005 and in the spring of WY 2006, but it has <br />been damp or dry for most of the period of record. Monitoring at this spring began in <br />1996. <br />3.2.2.4 Spring 15 -1 <br />Spring 15 -1 is located on the west side of an unnamed drainage tributary to the <br />North Fork of the Gunnison between Sylvester Gulch and Box Canyon (Map 2). This <br />June 2012 HydroGeo, Inc. <br />
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