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WSP04498
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Last modified
1/26/2010 12:55:43 PM
Creation date
10/12/2006 12:23:53 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8276.120
Description
Grand Valley Unit-Colorado River Basin Salinity Control Project
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
6/1/1983
Title
Supplement To Definite Plan Report: Stage Two Development Grand Valley Unit
Water Supply Pro - Doc Type
Definite Plan Report
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<br />to <br />cn <br />C:-,l <br />o <br /> <br />.--, <br /> <br />~~) <br /> <br />CHAPTER V <br /> <br />STAGE TWO PLAN OF DEVELOPMENT <br /> <br />For Stage Two, the Fish and wildlife Service is considering alter- <br /> <br />natives to the acquisition and development of lands. <br /> <br />Ideas inc lude <br /> <br />development of wildlife ponds on the desert side of the Government <br /> <br />Highline Canal, development of cross-drainage features for wildlife <br /> <br />habitat, deer escape devices along the canal, and voluntary on-farm <br /> <br />development of habitat along laterals. Final recommendations may include <br /> <br />a combination of land acquisition with the implementation of items <br /> <br />discussed above. <br /> <br />Geology and Construction Materials <br /> <br />Geology <br /> <br />The Mancos Shale is often overlain by various forms of alluvium; <br /> <br />however, it is either exposed or covered by only a few feet of soi 1, <br /> <br />especially in the western portion of the unit area. <br /> <br />The surficial <br /> <br />deposits are composed of fine-grained alluvium along washes and streams, <br /> <br />gravelly pediment materials, thin slopewash, residual soils, and a rather <br /> <br />extensive river channel deposit--the cobble aquifer. <br /> <br />Much of the proposed canal and lateral lining construction would <br /> <br />involve the weathered Mancos Shale. <br /> <br />This shale is hard and dense at <br /> <br />depth but near the surface is often fractured and jointed or weathered <br /> <br />into a lean clay or silty soil. <br /> <br />All excavation required during con- <br /> <br />struction along the canal and laterals, whether in soil or bedrock, would <br /> <br />be common excavat ions. <br /> <br />The shale contains secondary mineralization in <br /> <br />the form of gypsum and calcite and often slakes and cracks upon exposure <br /> <br />to the air. The upper weathered shale often contains ground water which <br /> <br />moves principally through joints, fractures, and open bedd ing planes. <br /> <br />43 <br />
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