My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2010-12-17_REVISION - C1981019 (153)
DRMS
>
Day Forward
>
Revision
>
Coal
>
C1981019
>
2010-12-17_REVISION - C1981019 (153)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 4:28:04 PM
Creation date
12/30/2010 10:50:25 AM
Metadata
Fields
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
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
150
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
Surface water 21 <br />l <br />0 4.3.1 Jubb Creek <br />Description <br />Jubb Creek is located on the eastern side of the Collom study area. Above the USGS <br />gaging station, it drains approximately 7.53 square miles of hilly plateau terrain. The <br />elevation of the stream channel ranges from about 6,400 ft amsl where it crosses Moffat <br />County Road 51 north of the Collom Syncline, to approximately 7,600 ft near the summit <br />of the Danforth Hills. The two forks of Jubb Creek (East and West) join at approximately <br />6,700 ft amsl (Figure 4.1). The stream channel runs in a northeasterly direction across <br />the Collom Syncline before joining Wilson Creek several miles northeast of the Trout <br />Creek Sandstone outcrop. <br />Historical flow data for Jubb Creek for the period 1975 through 1981 were collected at <br />USGS gaging station 9250610 (Figure 4.1). The flow data (provided in Appendix 4.B) <br />indicate that flow occurs from the spring through the fall, with maximum flow in May and <br />June. Jubb Creek generally has no flow during the winter. From December 2004 to <br />April 2005 flow ranged from approximately 5 to 110 gpm at sample location CJC. Flow <br />in Jubb Creek is partially controlled by several small stockponds located on both the <br />East and West Forks of Jubb Creek. At the time of monitoring, sediment transport was <br />low, as would be expected except during flood events. <br />Monitoring locations <br />C <br />The upper reaches of East and West Jubb Creeks are located within the footprint of the <br />proposed Collom Mine. Two sampling stations established in 1996 (EFJC and WFJC) <br />are located in the east and west forks of Jubb Creek, respectively (Figure 4.2). During <br />the pre - feasibility study, no surface water flow was observed at either location. To <br />monitor surface water quality downstream of the proposed mine, Jubb Creek sampling <br />location CJC, located at the confluence of East and West Jubb Creeks adjacent to valley <br />fill monitoring well MJ- 95 -03, was used. Samples were collected from all three locations <br />by KEC in 1996 and 1997. <br />4.3.2 Little Collom Gulch <br />Description <br />Little Collom Gulch is located near the center of the Collom study area. Above its <br />confluence with Collom Gulch, it drains approximately 2.9 square miles of hilly terrain. <br />The elevation of the stream channel ranges from about 6,520 ft amsl at the confluence <br />with Collom Gulch to approximately 7,800 ft amsl near the summit of the Danforth Hills. <br />The stream channel runs in a northeasterly direction through hilly terrain until it turns to <br />the west and joins the lower reach of Collom Gulch. <br />Little Collom Gulch is an ephemeral stream throughout its entire length. During the <br />period of December 2004 to April 2005, flow was not observed in Little Collom Gulch. <br />Several small stock ponds have been developed in the lower reach and have contained <br />water on occasion. <br />2572 -R2 colowyo Coal Company <br />Water Management Consultants <br />
The URL can be used to link to this page
Your browser does not support the video tag.