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<br />.. <br />I <br /> <br />, <br />II <br />I <br />.1 <br />:. <br />I <br />I <br />1:1 <br />, <br />, <br />;. <br />, <br />; <br />:1 <br />I <br /> <br />\1 <br /> <br />, <br /> <br /> <br />il <br />II <br />I <br />\ <br />.1 <br /> <br />j <br /> <br />'I <br />I <br />'I <br />1,1 <br />I <br />III <br />I <br />'I <br />'I. <br /> <br />along its length with the major ones--Park Creek and Spring <br /> <br />Gulch--joining Dry Creek in the upper third of the basin. <br /> <br />The channel is intercepted at two locations by major on-stream <br /> <br />reservolrs, Douglas Reservoir and Park Creek Reservoir (Figure 2). <br /> <br />Park Creek Reservoir is a fairly new U. S. Bureau of Reclamation <br /> <br />storage reservoir located high in the upper basin on the Park <br /> <br />Creek tributary to Dry Creek. The reservoir has a surface area <br /> <br />of approximately 190-acres and a tributary area of 3.8-square <br /> <br />miles. Douglas Reservoir is located on'Dry Creek in approximately <br /> <br />the middle of the basin. This reservoir has a surface area of <br /> <br />about 640-acres and a tributary drainage area of 44.0-square miles. <br /> <br />Historically, the Dry Creek Basin has been in agricultural land <br /> <br />use with a very active irrigation network. Over the past 30 <br /> <br />years, the basin has been experiencing development in the lower <br /> <br />reach below U. S. Highway 287. The development ln some cases <br /> <br />has obliterated the historic Dry Creek channel, particularly <br /> <br />in reaches near College Avenue. Commercial and light industrial <br /> <br />development is rapidly expanding ln the basin reach near the <br /> <br />confluence with the Cache la Poudre River in the area surrounding <br /> <br />Valley Airpark. The area immediately downstream of College <br /> <br />Avenue is currently experiencing residential development, and <br /> <br />commercial development continues to expand along College Avenue. <br /> <br />.~:.:t;~ <br />