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WSP06888
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Last modified
1/26/2010 2:24:49 PM
Creation date
10/12/2006 1:56:15 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8270.100
Description
Colorado River Basin Water Quality/Salinity -- Misc Water Quality
Basin
Colorado Mainstem
Water Division
5
Date
4/1/1982
Author
USDA
Title
Colorado River Water Quality Improvement Program - Final Environmental Impact Statement for Lower Gunnison Basin Unit - Montrose and Delta Counties CO and Uintah Basin Unit
Water Supply Pro - Doc Type
EIS
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<br /> <br /> <br />The area consists of several intermountain valleys and mesas drained by the <br />Uncompahgre and the Gunnison Rivers and their tributaries. The Continental <br />Divide through the Elk Mountains and the Cimmarron Ridge form the area's east <br />and southeast boundaries. The Grand Mesa forms the north boundary. The Uncompahgre <br />Plateau and the San Juan Mountains comprise the west and south boundaries, <br />respectively. <br /> <br />Physiography and Geology <br /> <br />The Lower Gunnison Unit contains two million acres. About 42 percent <br />of this area is privately owned and consists of 182,500 acres of irrigated <br />cropland including the 171,000 acres within the study area, and 663,500 acres <br />of nonirrigated rangeland. The irrigated land, mostly within the 0-2 and 2-5 <br />percent slope groups, developed from alluvium, glacial outwash and shale. <br />Forest land managed by ~he U.S. Forest Service makes up 36 percent of the area <br />and is considered a low producer of salts and sediment. Rangeland, highly <br />susceptible to erosion, managed by the Bureau of Land Management, comprises 22 <br />percent of the area. <br /> <br />Mancos shale underlies most of the valley surrounded by older Dakota sandstone <br />and younger volcanic rock as shown in Figure IV-2. The Mancos formation, a <br />marine shale with high salt content, consists mainly of gray silty clay. It <br />is the principal source of salt in the Lower Gunnison Unit. Salts are con- <br />centrated in certain areas within the shale and the younger alluvial deposits. <br />Lenses of crystalline salt often are exposed during excavation into shale. <br /> <br />Elevation in the area ranges from 4,550 feet above mean sea level where the <br />Gunnison River joins the Colorado River, to 14,300 feet on Uncompahgre Peak in <br />the southern end of the basin. Because of the arid climate below about 7,000 <br />feet elevation, salts have not been leached naturally from the soil. The <br />leaching process is greatly accelerated by applying irrigation water to these <br />salt laden soils. <br /> <br />Notable sites of scenic importance within the project area include Box Canyon, <br />the San Juan Mountains, Young's Peak--a chimney rock near Crawford--and the <br />Black Canyon of the Gunnison River. <br /> <br />Climate <br /> <br />The mean annual temperature at Delta is 510F and ranges from a mean <br />maximum temperature for July of 940F to a mean minimum temperature for January <br />of 140F. The mean annual temperature for all Lower Gunnison weather stations <br />is 49.60F. The average annual precipitation at Delta is 8 inches and 9 inches <br />at Montrose. About one half is in the form of winter snow. The average length <br />of the growing season is 146 days near Delta with elevation of 4,960 feet <br />above mean sea level and 152 days at Montrose, elevation 5,800. The estimated <br />length of growing season at Crawford and other locations at higher elevation <br />is about 105 days. The area below 6,200 feet elevation is characterized by <br />low precipitation, low humidity, abundant sunshine, and a wide range in annual <br />and daily temperatures. <br /> <br />Water Supply <br /> <br />Projects built by the Bureau of Reclamation supply water to 99,000 <br />acres, 54 percent of the irrigated land in the valley. The largest, the <br /> <br />IV-26 <br /> <br /> <br />
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