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PERMFILE47138
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PERMFILE47138
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Entry Properties
Last modified
8/24/2016 10:49:11 PM
Creation date
11/20/2007 1:03:31 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
X200521710
IBM Index Class Name
Permit File
Doc Date
8/29/2005
Doc Name
NOI Application
From
Bowie Resources LLC
To
DMG
Media Type
D
Archive
No
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Lower B, B-1, or Lower Somerset <br />4 to 12 ft thick, mined at King (old <br />where combined with Upper B <br />Interval, 5 - 30 ft <br />Bowie), and in places at Somerset <br />A, Old King, or Snowshoe <br />1 to 3 beds 0 to 6 ft thick, never mined significantly <br />Interval, 0-20 ft <br />Rollins Sandstone <br />Surface Water <br />The XPA is located on the north side of the valley of the North Fork of the Gunnison <br />River, known locally and less formally as the North Fork River. The North Fork is part of <br />the Colorado River system. It is a perennial stream, formed by the joining of Anthracite <br />Creek and Muddy Creek approximately nine miles east of the plan area, immediately <br />downstream from the Paonia Dam and Reservoir (located on Muddy Creek). The North <br />Fork joins the Gunnison River proper west of Hotchkiss, approximately 20 miles <br />southwest of the XPA. North Fork flow is partially regulated by Paonia Dam, and is <br />significantly diminished during irrigation season by numerous agricultural diversions. <br />Principle tributaries of the North Fork upstream from Terror Creek are Thompson and <br />• Hubbard creeks and Raven Gulch. Downstream tributaries are Minnesota, Roatcap, <br />Reynolds, Jay, Cottonwood, and Leroux creeks. In addition to Terror Creek, Hubbard, <br />Minnesota, Cottonwood, and Leroux creeks drain significant areas. <br />East of Paonia all of the watersheds are quite steep with high relief for such small <br />watershed areas. Except for Hubbard Creek and Terror Creek, defined channels have <br />not been extensively developed due to the resistance of the Mesaverde Group <br />sandstones. Ten to 20-ft drops over sandstone ledges are common. The elevation of <br />the East Fork of Terror Creek at the north boundary of the area is 8,400 feet and at the <br />south edge 7,250 ft, producing a gradient of about 9% for the 2.24 miles of the stream <br />within the XPA. <br />The XPA is drained by the West and East Forks of Terror Creek. According to existing <br />surface water inventories performed for the Ironpoint Tract Federal coal lease and <br />Bowie No. 2 mines, there are one pond and three springs in the eastern portion of the <br />XPA. The Bowie 7.5 minute Quadrangle Map indicates there is one additional pond and <br />one ditch located within the XPA. The pond is located west of the northwest comer of <br />section 31. The Julian Ditch enters the XPA in section 29. This ditch flows into the East <br />Fork of Terror Creek in the northeast corner of section 32. <br />Terror Creek Reservoir (a.k.a. Bruce Park Reservoir) is northeast of this XPA. This <br />reservoir is filled during spring runoff from waters diverted from a watershed near the <br />Overland Reservoir and a diversion ditch known as the Hubbard Creek Extension of the <br />• Holy Terror Ditch. <br />
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