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PERMFILE120668
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PERMFILE120668
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Entry Properties
Last modified
8/24/2016 10:19:18 PM
Creation date
11/25/2007 8:39:25 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981016
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
Main permit narrative
Media Type
D
Archive
No
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III.D. Human and Natural Resources <br />• 1. Local Topography <br />The leases that make up the Hawk's Nest Mine permit area lie along the <br />North Fork Gunnison River, approximately 1 1/2 miles east of Somerset, Colorado. <br />These leases extend generally north of the North Fork Gunnison River. Eleva- <br />tion varies from 6,140 feet along the North Fork River to over 8,200 feet on <br />the northern edge of the leases, all on the south-facing valley slopes which <br />define the North Fork river drainage. North of this lease line the slopes rise <br />steeply to over 8,600 feet before breaking to uneven park and hill landscape <br />which constitutes the eastern extension of Grand Mesa. <br />Along this portion of the North Fork Gunnison River, the river is narrowly <br />confined by the steep slopes of Grand Mesa to the north and the West Elk Moun- <br />• tains to the south. The permit area lying north of the North Fork consists of <br />a series of east-west trending ridges which are separated by incised gulches <br />or canyons containing ephemeral or intermittent streams. These drain south <br />into the North Fork Gunnison River. <br />The maximum relief on the permit area is generally found along the sand- <br />stone escarpments which form the step-like ridges. Here slopes may reach 90 <br />degrees vertical. The average slope across the lease area is approximately <br />40 percent (sae 1" = 500' map Appendix D and Figure III.B-1). <br />The landforms present on the permit area are largely the result of the <br />differential erosion of the Mesa Verde Formation (sedimentary rock strata). <br />Thick resistant sandstones form vertical to steep cliffs and escarpments. <br />Shales and other less resistant beds form gentle slopes between the cliffs <br />• and ledges. Because of the predominance of sandstones in the Mesa Verde <br />42 <br />
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