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2010-12-17_REVISION - C1981019 (153)
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2010-12-17_REVISION - C1981019 (153)
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Last modified
8/24/2016 4:28:04 PM
Creation date
12/30/2010 10:50:25 AM
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Template:
DRMS Permit Index
Permit No
C1981019
IBM Index Class Name
REVISION
Doc Date
12/17/2010
Doc Name
Exhibit 7 Item 21 Collom Project Pre-Feasibility Hdyrology Report
Type & Sequence
PR3
Email Name
JRS
Media Type
D
Archive
No
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22 <br />r <br />0 Monitoring locations <br />Surface water <br />The upper reaches of Little Collom Gulch are located within the proposed Collom Mine. <br />As a result, an upgradient monitoring station was not established. <br />Sampling Point LLCG is located immediately adjacent to valley fill well MLC -04 -01 east <br />and just above the confluence of Little Collom and Collom Gulches (Figure 4.2). <br />4.3.3 Collom Gulch <br />Description <br />Collom Gulch is located near the center of the Collom study area. Above sampling point <br />LCG, it drains approximately 5.05 square miles of hilly terrain. The elevation of the <br />stream channel ranges from 6,457 ft amsl where it crosses Moffat County Road 51 to <br />greater than 7,800 ft amsl near the summit of the Danforth Hills. The stream channel <br />runs north - northeast through the Collom Syncline and then across the pediment slope <br />north. of the syncline before joining Morgan Gulch. Collom Gulch is an intermittent <br />stream through out its entire length. <br />The upper and lower reaches of Collom Gulch flow in a relatively narrow valley. The <br />middle reach flows in a flat, wide valley bottom just south of the synclinal axis. There is <br />little sinuosity developed except in the middle reach where the channel is braided. <br />10 In December 2004, January 2005, and February 2005, there was no flow at the upper <br />Collom Gulch sampling point (UCG). Flow at the lower Collom Gulch sampling point <br />(LCG) ranged from 2.6 gpm in December 2004 to about 30 gpm in February 2005. Flow <br />began to increase in the spring due to snowmelt and increased precipitation. In April <br />2005, stream flow at the upper Collom Gulch station was about 340 gpm whereas flow at <br />the lower Collom Gulch station was about 90 gpm. This indicates that snowmelt in the <br />upper reach is infiltrating into the Collom Gulch valley fill during the spring. In the <br />summer and fall, this recharge probably contributes to stream flow in lower Collom Gulch <br />as groundwater discharge to the stream. <br />Monitoring locations <br />Sampling point UCG is immediately adjacent to valley fill well MC- 04 -01. Sampling point <br />LCG is immediately adjacent to valley fill well MC -04 -02 (Figure 4.2). <br />4.3.4 Straight Gulch <br />Description <br />Straight Gulch is located on the western edge of the Collom study area. Above sampling <br />point LSG, it drains approximately 7.51 square miles of hilly terrain. The elevation of the <br />stream channel ranges from 6,639 ft amsl at the confluence of Straight Gulch and <br />Morgan Gulch to approximately 7,800 ft amsl near the summit of the Danforth Hills. The <br />( stream channel runs north - northeast across the south limb of the Collom Syncline and <br />0 merges with Morgan Gulch south of the synclinal axis. <br />2572 -R2 Colowyo Coal Company <br />Water Management Consultants <br />
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