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WSP10235
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Last modified
1/26/2010 2:57:54 PM
Creation date
10/12/2006 4:13:53 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8281.910
Description
Colorado River Studies and Investigations -- Grand Valley Salinity Study
Basin
Colorado Mainstem
Water Division
5
Date
12/1/1976
Author
Soil Cons Serv
Title
Grand Valley Salinity Study - draft
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />~ <br />.....j <br />N <br />.:,:) <br />~,-," " <br />~ <br /> 2 <br /> 3 <br /> 4 <br /> 5 <br /> 6 <br /> 7 <br /> 8 <br /> 9 <br /> 10 <br /> II <br /> 12 <br /> 13 <br /> 14 <br /> 15 <br /> 16 <br /> 17 <br /> 18 <br /> 19 <br /> 20 <br /> 21 <br /> 22 <br /> 23 <br /> 24 <br /> 25 <br /> <br />.~ <br /> <br />Four irrigation entities divert water from the Colorado River. These <br /> <br />Include the Grand Valley Water Users Association (Bureau of Reclamation <br /> <br />Project), Grand Valley Irrigation Company, Palisade Irrigation District, <br />and Mesa County Irrigation District. A fifth irrigation company, the <br /> <br />Redlands Power.and Water Company, diverts water from the Gunnison River. <br /> <br />A ~umber of other small companies have carriage agreements with the <br /> <br />major canal companies for delivery of water. <br /> <br />First irrigation in the valley began in 1882 with the construction <br /> <br />of what is now the Grand Valley Canal (~rand Valley Irrigation Company). <br />Other private systems were built during the period between 1882 and 1908. <br /> <br />Construction of the last major system, the Grand Valley Project under <br /> <br /> <br />the Reclamation Service, began in 1908 with the major construction <br /> <br />completed in 1926. This project consists of two divisions, t.he Garfield <br /> <br />Gravity and the Orchard Mesa Divisions, on the north and south sides of <br /> <br />the river, respectively. <br /> <br />The soils of this general area are derived from the Mancos Shale <br /> <br />formation. This marine formation has a very high salt content and <br /> <br />ground water percolating over and through the shale picks up high concen- <br /> <br />trations of salt which are transported to the Colorado River through <br /> <br />wasteways, ditches, or by natural ground water movement to the river. <br /> <br />Because of the arid climate, these salts have not been leached naturally, <br /> <br />and high quantities remain. Lenses of white crystalline salts are often <br /> <br />exposed during excavation operations. The Mancos formation consists of <br /> <br />3,000 to 5,000 feet of relatively uniform silty clay shale with veinlets <br /> <br />of gypsum, calcite, and sodium sulphate. <br /> <br />14 <br /> <br />\, <br /> <br />
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