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PERMFILE48881
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PERMFILE48881
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Entry Properties
Last modified
8/24/2016 10:50:48 PM
Creation date
11/20/2007 1:48:40 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981033A
IBM Index Class Name
Permit File
Doc Date
11/14/2003
Section_Exhibit Name
Rule 2.04 Environmental Resources
Media Type
D
Archive
Yes
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• 2.04.7(1 )(iii) <br />Monitoring data for the Lone Pine Gulch springs discussed <br />below are presented on page 2.04-30ii through 2.04-30vi. The location of the springs <br />are shown on Map 6. <br />Spring G-26, also know as spring G-26A, has been <br />monitored intermittently since 1975. The spring flows intermittently. This spring has <br />been effected by past landslides. It could be characterized as a spring fed stock pond. <br />The monitoring data indicates the spring will exhibit high flows in May and June. <br />Spring G-26B has also been effected by landslides. This <br />spring apparently supplied water to some old cabins below it which are now in ruins. <br />Spring G-26C was a new monitoring point in 1997. It emerged below spring G-26B in a <br />slide or slough area. Apparently the flow from G-26B is emerging as G-26C <br />Monitoring point CR-12 is a spring located in the bottom of <br />Lone Pine Gulch. <br />Lone Pine Gulch is an ephemeral drainage that would only <br />• flow during significant precipitation events. There is no monitoring data available for <br />Lone Pine Gulch. <br />On November 17, 1997 the DMG was notified of a slide that <br />is located immediately west of the reclaimed Bear No. 3 Mine portals. The slide <br />became active on Saturday, November 15th. Debris from the slide flowed onto the old <br />coal stockpile pad (west of the the reclaimed stacking tube) and into the North Fork of <br />the Gunnison River south of the mine access bridge. Shortly after the slide occurred, <br />water started flowing from the east side of the slide scarp. This spring has been <br />monitored since late in 1997. The maximum flow from the spring has bee about 30 <br />gallons per minute. Typical flows are less than 20 gpm. The pH of the spring water is <br />about 7.0 and the conductivity is about 4500 umhos/cm. <br />(iv) A water rights listing from Division 4 and a water rights <br />location map is included in the permit as Table 12 and Figure 6. <br />/~R-a s <br />C~-oti) <br />/~ /PRove/~ 1~~14Jo3 <br />2.04-29b <br />Rev. 11 /02 <br />
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