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1994-12-29_GENERAL DOCUMENTS - C1980007
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1994-12-29_GENERAL DOCUMENTS - C1980007
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Last modified
2/6/2021 10:59:04 PM
Creation date
11/23/2007 11:13:31 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
General Documents
Doc Date
12/29/1994
Doc Name
Decision Doc Federal Lease
Permit Index Doc Type
Other Permits
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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wetherill Milkvetch (Astragalus wetherillll) Category-2 <br /> Columbian sharptailed Grouse (Tympanuchus phasianellus) Category-2 <br /> Roundtail chub (Oil& robusta) Category-2 <br /> • Category 1 and 2 species are candidates for listing as <br /> threatened or endangered under the Endangered Species Act; <br /> information is currently not sufficient to support listing. <br /> Proposed species are those which have been formally proposed <br /> to be listed as threatened or endangered under the Endangered <br /> Species Act. Proposed species are afforded the same <br /> protection as listed species. <br /> H. Cultural Resources <br /> There have been two cultural resource inventories conducted for <br /> exploration drill holes in 1992. No sites were found. There <br /> will be another survey conducted for additional drill sites in <br /> 1993 . <br /> I. Water Resources <br /> Surface Water <br /> The tract is located within the North Fork of the Gunnison River <br /> (North Fork) Drainage Basin. The area, located a few miles south <br /> of the North Fork mainstem is a topographic high, averaging 7600 <br /> feet above MSL, on the northern flanks of Jumbo Mountain, and is <br /> drained by several first and second order intermittent channels. <br /> • These channels enter the North Fork approximately 5 miles <br /> upstream (east) of the town of Paonia, Co. The flow of the North <br /> Fork varies seasonally, with high flows occurring during spring <br /> from snowmelt. After snowmelt, flows begin to recede, reaching <br /> their low during winter. The 100-year flood event produces a peak <br /> flow rate of about 7,920 cubic feet per second. <br /> Water quality data (inorganic constituents and suspended sediment <br /> concentrations) for the North Fork indicates that generally, <br /> water quality is good. The water is an alkaline, soft, calcium- <br /> bicarbonate-sulfate type with total dissolved solids <br /> concentration averaging around 100 mg/l. The water is cold, with <br /> winter temperatures near freezing and summer temperatures in the <br /> 18-20 degree C range. Suspended solids concentration averages <br /> near 50 mg/1 with maximum concentrations occurring during <br /> snowmelt, in the range of 200-250 mg/l. Both dissolved metals <br /> and nutrient concentrations are generally low throughout the <br /> year. <br /> Surface water flow over the tract is in response to snowmelt and <br /> summer precipitation events. There is one known developed water <br /> source (Jumbo Mountain spring 12) on the tract (BIM surface) and <br /> three others (Jumbo Mountain Springs f 1, 3,i 5) within a mile of <br /> the tract boundary (see Map 4) on BLM surface. The primary use of <br /> these water sources is livestock and wildlife. The BLM has <br /> • reserved water rights on these water sources, adjudicated by the <br /> State of Colorado, with an appropriation date of April 17, 1926. <br /> Page 10 <br />
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