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REP19622
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REP19622
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Entry Properties
Last modified
8/24/2016 11:48:17 PM
Creation date
11/27/2007 2:41:42 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981034
IBM Index Class Name
Report
Doc Date
1/31/1994
Doc Name
ANNUAL HYDROLOGIC REPORTS PN C-81-034
From
MINREC INC
To
DMG
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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MINREC, INC. <br />2768 COMPASS DRZVE, SUITE 101 <br />GRAND JUNCTION, COLORADO 81506 <br />PRONE: (303) 245-4101, FAR 242-7908 <br />RED CANYON MINES <br /> <br />January 28, 1994 <br />i' F-' i <br />C. E. Johnston ~n.rd 31 1°34 <br />Division of Minerals and Geology <br />1313 Sherman St., Room 215 - .__,~„~,_„ <br />Denver, CO 80203 <br />Re: Annual Hydrologic Reports <br />Permit C-81-034 <br />Dear Ms. Johnston: <br />The Divisions letter dated December 13, 1993, transmitted its <br />comments on Minrec's 1992 and 1993, Red Canyon Mine, Annual <br />Hydrologic Reports. Following are Minrec's responses to those <br />comments <br />Surface Water <br />The Division noted that the conductivity measurements taken during <br />September on Ward Creek, increase significantly from the upstream <br />to the downstream sampling point. I do not believe the available <br />monitoring data supports this observation. Enclosed is a table <br />titled Ward Creek Late Season Flows. This table shows, for the <br />period of record 1982 - 1993, the average increase in conductivity <br />between the upstream and downstream monitoring points is 159 <br />umhos/cm. The comparable increase in the conductivity measurement <br />for both 1992 and 1993 is 150 umhos/cm which is actually just below <br />the historic average increase. <br />Also enclosed is a graph of the conductivity measurements for <br />upstream and downstream Ward Creek taken during from 1982 through <br />1993. This graph supports the conclusion that the conductivity in <br />lower Ward Creek is following historic trends. <br />Minrec will continue monitoring Spring 1 and Spring 3 to observe <br />whether the conductivity continues to increase. It should be noted <br />that both Spring 1 and Spring 3 have recorded historic high <br />conductivity measurements when they were also exhibiting historic <br />high flows. The historic high for Spring 1 occurred May 26, 1983; <br />990 umhos/cm at 35 gpm. The historic high for Spring 3 occurred <br />September 18, 1993; 750 umhos/cm at 6 gpm. <br />Minrec will continue to monitor Ward Creek in accordance with <br />permit requirements. However, there is no indication the <br />
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