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<br />I <br /> <br />I <br /> <br />I <br /> <br />E. Water Storage and Conveyance Features Studied <br /> <br />I <br /> <br />I <br />I <br /> <br />Several reservoir locations were investigated for use in the <br />development of alternatives. Some of these alternatives have been <br />investigated previously by the United States Bureau of Reclamation <br />(USBR) or other engineers, while other sites have never been formally <br />investigated. These dam and reservoir locations are shown in Figure <br />I-I and briefly described below. <br /> <br />Lower Kendig <br /> <br />On West Divide Creek below the Highline Ditch <br />Diversion. Same site as the USBR's Kendig Dam <br /> <br />I <br /> <br />Upper Kendig <br /> <br />On West Divide Creek above the Highline Ditch <br />Diversion. This site was included so releases <br />could be made to the Highline Ditch wi thout <br />pumping. <br /> <br />I <br /> <br />I <br /> <br />Haystack <br /> <br />On Upper West Divide Creek. This is a site on <br />the main stem and not the offstream site stu- <br />died by the USBR in 1963 and 1964. <br /> <br />I <br />I <br /> <br />Dry Hollow <br /> <br />On lower Dry Hollow Creek; this is the same <br />site as that studied by the USBR. <br /> <br />I <br /> <br />East Divide Creek <br /> <br />On the lower reaches of East Divide Creek <br />above the diversion points of the major <br />ditches. This site has not previously been <br />formally investigated. <br /> <br />I <br /> <br />Upper Mamm <br /> <br />On the upper reaches of West Mamm Creek. This <br />site has never before been formally <br />investigated. This reservoir can service the <br />upper and lower halves of Hunter Mesa. <br /> <br />I <br /> <br />I <br />I <br /> <br />Lower Mamm <br /> <br />On West Mamm Creek just upstream of its <br />confluence with Middle Mamm Creek and East <br />Mamm Creek. This reservoir can service the <br />lower half of Hunter Mesa. <br /> <br />Upper Beaver <br /> <br />On the upper reaches of Beaver Creek. This <br />site, which has not been previously studied, <br />uses a glacial morrain as part of the <br />impoundment. <br /> <br />I <br /> <br />I <br /> <br />1-7 <br /> <br />I <br />