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PERMFILE57005
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PERMFILE57005
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Entry Properties
Last modified
8/24/2016 10:59:26 PM
Creation date
11/20/2007 5:16:28 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980005A
IBM Index Class Name
Permit File
Doc Date
5/20/2005
Section_Exhibit Name
Tab 7 Hydrology
Media Type
D
Archive
Yes
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State Reg. <br />II. SURFACE WATER INFORMATION • <br />As illustrated on Exhibit 7-3, the Seneca II Mine lies within the drainages <br />of Little Grassy Creek, Grassy Creek, and two unnamed tributaries of <br />Fish Creek. These drainages are part of the Yampa River System which <br />in turn lies in the Upper Colorado River Basin. Seneca Coals, Ltd. has <br />obtained baseline information in terms of quantity and quality on the <br />Yampa River and Fish Creek (upstream and downstream from mining) <br />from government agencies. In addition, Seneca Coals, Ltd. has estab- <br />lished abaseline monitoring program on the drainages that are in the <br />direct vicinity of the mine. The following discussion gives quantity and <br />quality information for each of these basins and relates this information <br />to effluent from the mine. <br />A. Yampa River Basin <br />Like other rivers in the Upper Colorado River Basin whose source lies <br />along the Continental Divide, snowmelt is the principle source of water <br />for the Yampa River and most of its tributaries. According to lorns et <br />al. (1965), summer precipitation has little effect on the discharge of <br />principal streams. The base flow of the streams draining the high moun- <br />tain areas is uniform for nine months of each year with April, May, and <br />June showing substantially higher flows. The streams draining the areas <br />of lower altitudes in the central and western part of the basin are pri- <br />marly intermittent. <br />Figure 7-6 shows a typical hydrograph for the Yampa River near the <br />mountains at Steamboat Springs. High flows between 200 and 1,500 cfs <br />occur between the beginning of April and the end of June. Further <br />downstream east of Hayden near the discharge of Grassy Creek peak <br />flow also occurs during the spring. This is illustrated in Figure 7-7 for <br />the 1979 water year. As expected, there is more flow at the Hoyden <br />station. <br />Seasonal variation in water quality also occurs. During months of high • <br />water in the spring and early summer, the concentrations of total dis - <br />7-54 <br />Revised 5/27/81 <br />
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