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<br /> <br />Mail: <br />Colorado Geological Survey, <br />1313 Sherman Street, <br />Room 715, Denver, CO 80203 <br />Phone: (303) 866-2611 <br /> <br />New CGS Website address: <br />http://geosurvey.state.co. us <br /> <br />Fax: (303) 866-2461 <br />E-mail: <br />cgspubs@state.co.us <br /> <br />VISA@ and MasterCard@ <br /> <br />1:::41:1.-1 <br />accepted. <br />Prepayment required. <br /> <br />....... ....... .......... <br /> <br />SHIPPING AND HANDLING <br /> <br />.................................. <br /> <br />Please contact the CGS for <br />shipping and handling costs. <br /> <br />Discounts <br />Available on bulk orders. <br /> <br />Call for a complete <br />publication list <br /> <br />.. ...... ....... ...... ... <br /> <br />Related <br />Publications <br /> <br />Bulletin 36 <br />Geologic Control of Supply and Quality <br />of Water in the Mountainous Part of <br />Jefferson County, Colorado $2.00 <br /> <br />Bulletin 42 <br />Water Resources of Boulder Countyl <br />Colorado $4.00 <br /> <br />Information Series 37 <br />Water Resources Beneath State Lands <br />in Port of T. 16 S., R. 63 W., Block <br />Squirrel Creek Basinl EI Paso County, <br />Colorado $10.00 <br /> <br />Informatian Series 48 <br />C%rado Water Quo/ity Database <br />from the Environmental Protection <br />Agency's STOREr Database $20.00 <br /> <br />publications continued on p. 14 <br /> <br />6 <br /> <br />- <br /> <br />listed below, are illustrated on the <br />map on page 4: South Platte, <br />Republican, Arkansas, Colorado, <br />Yampa, While, Gunnison, San <br />Juan, Dolores, and Rio Grande. <br />Sedimentary rock aquifers are <br />composed of consolidated clastic <br />and carbonate deposits. Ground <br />water in sedimentary rock aquifers <br />can be either confined or uncon- <br />fined. The major sedimentary rock <br />aquifers in Colorado consist pre- <br />dominantly of sandstones and <br />limestones of varying age. Many <br />of these aquifers are located in <br />structural basins that contain mul- <br />tiple geologic units/aquifers. <br />Large quantities of ground water <br />occur in deep basins such as the <br />Denver Basin and in the flat-lying <br />High Plains Aquifer of eastern <br />Colorado. Basin-wide aquifer sys- <br />tems, illustrated on the map on <br />page 5, include the: Denver, Pic- <br />eance, Paradox, San Juan, Eagle, <br />Raton, and Sand Wash Basins; and <br />North and Middle Park, South <br />Park, and H uerfano Park. <br />The intermontane valleys of <br />central Colorado contain a net- <br />work of hydraulically intercon- <br />nected aquifers within valley-fill <br />deposits. These unconsolidated to <br /> <br />RockTalk <br />is published by the <br />Colorado Geological Survey <br />1313 Sherman Street, <br />Room 715, Denver, CO 80203 <br /> <br />Back issues and subscriptions <br />can be obtained FREE by contact- <br />ing CGS by mail, fox, phone, or e- <br />mail or download them from our <br />Web site. <br /> <br />Phone: (303) 866-2611 <br />Fax: (303) 866-2461 <br />E-mail: cgspubs@state.co.us <br />Web site: <br />http://geosurvey.state.co.us <br /> <br />THIS ISSUE <br />Editor: Matt Sares <br />Production: Cheryl Brchon <br />Illustrations: larry Scott <br /> <br />- <br /> <br />poorly-consolidated aquifers con- <br />sist of sediments that were <br />deposited by wind, water, and <br />gravity, such as landslides from <br />erosion of the surrounding moun- <br />tain ranges. Similarly, the Great <br />Plains of eastern Colorado are <br />underlain by a thick sequence of <br />gravel, sand, silt, and clay that <br />was eroded from the Rocky Moun- <br />tains. These poorly-consolidated, <br />often localized, sedimentary <br />aquifers include the San Luis Val- <br />ley, Wet Mountain Valley, and <br />High Plains Aquifer. <br />Lastly, Colorado's crystalline <br />rocks are exposed at the surface in <br />the west-central portion of the <br />state (see map on page 4). The <br />crystalline rocks throughout this <br />province are Precambrian-aged <br />igneous and metamorphic rocks; <br />largely granites, gneisses, and <br />schists; and geologically recent <br />(Tertiary age) volcanic and igneous <br />intrusive rocks. Ground water in <br />crystalline-rock aquifers is general- <br />ly unconfined, and occurs where <br />joints, fractures, and faults have <br />crosscut the rock. These rock types <br />occupy approximately 19 percent <br />of the state's total area, and repre- <br />sent the fractured, crystalline-rock <br />aquifers that supply much of the <br />domestic water-supply needs in <br />the mountainous portion of our <br />state. <br />As Colorado's population <br />grows, the importance and use of <br />ground water also grows. The <br />CGS is in the process of compiling <br />a Ground Water Atlas of Colorado <br />tha t will describe each of these <br />major aquifers or aquifer systems, <br />addressing individual hydrogeo- <br />logic units, their hydraulic charac- <br />teristics, principal water uses and <br />withdrawals, and a brief look at <br />water quality. When complete in <br />early 2003, this atlas will provide <br />important information useful to <br />farmers, ranchers, homeowners, <br />businesses, and decision-makers <br />in Colorado. <br /> <br />~ <br /> <br />!' <br /> <br />p <br /> <br />-Ralf Topper <br /> <br />Colorado Geological Survey ROCKTALKVol. 5, No.4 <br />