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<br />:;!' ,~ <br /> <br />"" <br /> <br /> <br /> <br />Complete documentation of literature search is found in the <br />Appendix of this report (see "Record of Literature Search"). <br /> <br />I As a result of this literature search several hydrologic analyses <br />were found covering the study streams. _ Several analyses <br />conducted by the Bureau of Reclamation in 1967 (refer to appendix <br />of this report) as part of their work on the Arkansas-Fryingpan <br />Project included frequency studies of Lake Creek and the Arkansas <br />River in or near the study area. Due to l~ years of additional <br />gage records, the frequency analyses were recalculated for this <br />report. <br /> <br />In addition the U.S. Forest Service has operated a precipitation <br />- runo ff network within the Lake Creek bas in from 1965 - 1977. <br />This network included monotoring of precipitation and runoff <br />flows at five locations in the upper Lake Creek Basin with stream <br />gages on the North and South Forks, Lake Creek, and Sayres <br />Gulch. Since this information has never been published, covers a <br />relatively short period of record and covers only the upper areas <br />of the watershed much farther upstream of the study site, it was <br />not useful in this study. Refer to the Appendix of this report <br />for information supplied by the Forest Service. A map showing <br />the gage locations is included in the Appendix of this report. <br /> <br />DRAINAGE BASIN CHARACTERISTICS <br /> <br />Lake Creek <br /> <br />Lake Creek originates in Everett, Colorado, at the confluence of <br />the North and South Forks of Lake Creek. The headwaters are <br />located in San Isabel National Forest at elevations in excess of <br />13,500 feet. Lake Creek flows from its origin 7.5 miles to Twin <br />Lakes Reservoir and then to its confluence with the Arkansas <br />River at Balltown, Colorado. The drainage basin is shown on <br />Figure 2. <br /> <br />Lake Creek being part of the Arkansas-Fryingpan Project (see <br />description in Appendix) includes a major flow diversion into the <br />watershed from the Colorado River Basin through the Twin Lakes <br />Reservoir and Canal Company Tunnel Number 1. This ~iversion is <br />located in the headwater areas of Lake Creek approximately 4.5 <br />miles upstream of the study site. A USGS/State of Colorado <br />streamgage (07084500) on Lake Creek upstream of Twin Lakes <br />Reservoir and located approximately 3.0 miles downstream of the <br />study site has been operational since 1941. Tunnel flows have <br />been monitored by the State of Colorado since 1935. In addition, <br />a snowfence monitoring study conducted by the U.S. Forrest <br />Service (Refer to previous section) was conducted from 1965 <br />1977 . <br /> <br />()k, ~(/t .jpf ~ -W cJL -htf.?(yP - /4 & .knn <br />~~ ~d? ;P~.71W!~/~ <br />~<:~~ JtVM?~-h&. <br /> <br />o <br />