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<br />Ii Ul i) i'} ,~ <br /> <br />1f~~i~Il3 <br /> <br />;&.\.Wf..~W'l /' <br />3~,.~-:t.*,:<; <br /> <br />lnterio <br /> <br /> <br />United States Department of the <br /> <br />GEOLOGICAL SURVEY <br />Box 25046 <br />Denver Federal Center <br />Denver. Colorado 80225 <br /> <br />Water Resources Division <br />.Colorado District <br />Mail Stop 415 <br /> <br />IN REPLY REFER TO; <br /> <br />RElCt' . - <br />l...; ._ -.I.", <br />~I ' . <br />,vOV ".:.- <br />1 fj 1976 <br /> <br />CONS;:" It'..~ <br />'.ill", 11 <br />"MINING" OF ARAPAHOE AQUIFER OCCURRING IN ENGLEWOOD- GAlli) <br />CASTLE ROCK AREA <br /> <br />November 5, 1976 <br /> <br />INFORMATION FOR THE PRESS <br /> <br />SUBJECT: <br /> <br />RELEASE DATE: Immediately <br /> <br />FOR ADDITIONAL INFORMATION CONTACT: <br /> <br />J, E. Biesecker, District Chief <br />U.S. Geological Survey, WRD <br />Colorado District, Mail Stop 415 <br />Box. 25046, Denver Federal Center <br />Lakewood, Colorado 80225 <br />Telephone: 234-3815 <br /> <br />Increasing use of water from the artesian Arapahoe aquifer, principally <br />along Interstate Highway 1-25 in the Englewood-Castle Rock area, has <br />caused the potentiometric surface (the level to which water will. rise in <br />a well) to decline more than 200 feet in some parts of the area between <br />1965 and 1975, according to a recent U.S. Geological Survey, Department <br />of the Interior, report. <br /> <br />The 32-page report, complete with detailed maps, describes the physical <br />and hydraulic characteristics of the Arapahoe aquifer and the chemical <br />characteristics of tne water in the area. <br /> <br />Prepared in cooperation with the Colorado Division of Water Resources, <br />Office of the State Engineer, the report notes that the potentiometric <br />surface has declined throughout the area from 1965 to 1975. The decline <br />indicates that the aquifer is being "mined"; that is, discharge from the <br />aquifer, principally by wells, exceeds recharge to the aquifer from all <br />sources. Most artesian wells penetrating the aquifer that flowed prior <br />to 1975 have ceased flowing. Only one flowing well, with an estimated <br />flow of 3 gallons per minute, was observed ~uring the study. <br /> <br />,.O,-UTIO/\, <br /> <br />Q;-~<<;~(> <br />.... ~ <br />.., '-' <br />() m <br />a '" <br />~ ~ <br />-Yl.- ~ <br />';0'6-191" " <br /> <br />:~~~j <br />I <br /> <br /><i<i~ <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />...',i, <br />~~{ <br />~'Z:" <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />,.~:-"f-:c'''' <br /> <br /> <br />I <br />. ~i~I <br />',..--- <br /> <br />:;.-:':f:~-'-; <br />?;:~,,:"" <br /> <br />:~.,:.;.;.: - <br /> <br />:'."t;..'.::'::" <br /> <br />:';:"'" . <br />-:.}?? <br /> <br />:~?o:":-:> <br />