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<br />I <br /> <br />I <br /> <br />I <br /> <br />II <br /> <br />II. INTRODUCTION <br /> <br />The analysis within this report is based on a set of seven years <br /> <br />I <br /> <br />(1966-1972) of detailed daily averages of streamflow at seven tribu- <br /> <br />taries to Gore Creek. The location of stream gages is shown on the <br /> <br />I <br /> <br />reference terrain maps in both Figs. 1 and 2. <br /> <br />I <br /> <br />Temperature and precipitation data were not available within the water- <br /> <br />I <br /> <br />shed area and have been estimated from other reference location~ several <br /> <br />of which are identified in Figs. 1 and 2. <br /> <br />I <br /> <br />Hourly observations. of precipitation and streamflow, plus daily preci- <br /> <br />I <br /> <br />pitation values occurring in the San Juan mountains area of southwestern <br /> <br />Colorado, also have been used to develop summer time potential runoff <br /> <br />I <br /> <br />from thunderstorms in July and August in contrast to general storms <br /> <br />which are important in southwestern Colorado during September and <br /> <br />I <br /> <br />October. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />-3- <br />