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Last modified
1/26/2010 12:33:07 PM
Creation date
10/11/2006 10:40:40 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8271.200
Description
Colorado River Basin Salinity Control Program - Development and History - UCRB 13a Assessment
Basin
Colorado Mainstem
Water Division
5
Date
10/1/1979
Title
The Availability of Water for Oil Shale and Coal Gasification Development in the Upper Colorado River Basin - Summary Report
Water Supply Pro - Doc Type
Report/Study
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<br />N <br />W <br />W <br />o <br /> <br />in anyone year (day-to-day fluctuations are also common). As a function <br />of the precipitation patterns noted above, runoff from snowmelt during <br />the spring and summer months with 65 to 75 percent of the annual total <br />arising, on the average, during the period April through July (see fig. <br />2.5) . <br /> <br />Fish and wildlife resources are important components of the Upper <br />Colorado River Region's natural environment. The Region supports out- <br />standing, although inherently fragile, fish and wildlife habitats. <br />Sport fishing is especially important, attracting thousands of people <br />each year. Game animals also attract thousands of visitors and residents <br />alike, making hunting an impor<snt economic contributor to the Region. <br />Finally, the humpback chub, bony tail chub, and Colorado River squawfish <br />are on the Federal endangered species list in this Region. <br /> <br />Oil Shale and Coal Resources <br /> <br />The Green River Formation is the geologic source of the most abundant <br />oil shales in the United States (see fig. 2.6). Deposition of these oil <br />shales occurred in a lacustrine (lake) environment. The three ancient <br />lakes in which the Green River Formation was deposited were stable, two- <br />layer lakes which did not overturn annually as most lakes do, probably <br />because of their great depth. The resulting thermal and chemical char- <br />acteristics of the lake allowed the deposition of thin-bedded oil shales <br />and of a number of relatively rare carbonate minerals which occur through- <br />out the formation. <br /> <br />The chemistry of deposition is extremely complex. The organic matter <br />that was deposited has become kerogen. The additional minerals include <br />nahcolite, a sodium bicarbonate material which could be used as a source <br />of soda ash or which could find a market as is for use in air pollution <br />control devices. A second mineral is dawsonite, which could become a <br />source of alumina rivaling bauxite deposits in the United States. In <br />southwestern Wyoming, a third metal, trona, is currently being mined <br />commercially to produce soda ash. Finally, halite, a common salt, is <br />also abundant in the deposits. <br /> <br />It is difficult to accurately estimate the total amount of the Upper <br />Basin's oil shale resource, but geologists generally agree that it is <br />vast. The Green River Formation is estimated to contain more than 3 <br />trillion barrels of oil-equivalent in-place. In Colorado, continuous <br />oil shale sections 15 to 2,000 feet thick, averaging at least 15 gallons <br />per ton (gpt), exist under 1,380 square miles. These sections contain <br />richer portions averaging 25 gpt that represent 400 billion barrels <br /> <br />2-7 <br />
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