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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I I <br />I <br /> <br />high precipitation days recorded at Telluride, Durango and Silverton weather stdtians in the <br />late summer at the San Juan basin for 1964 - 1974 period. Precipitation at Gunnison, <br />Crested Butte and Cochetopa Creek weather stations for the same days were tabulated and <br />used for correlation. Data from individual stations from the two basins were correlated with <br />each other. The mean precipitation data for the three stations from each basin were also <br />correlated with each other. Results of these correlatians are presented in Table 7. <br /> <br />Based on the coefficient of correlations obtained from different correlations it can <br />be concluded that major storms on San Juan basin do not produce simi lar results in Gunni- <br />son Basin. <br /> <br />-4- <br /> <br />