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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 <br />I <br /> <br /> <br />" <br /> <br />Bould<;r <br />\F x / <br />7.6' { <br />I <br />I <br /> <br /><4" <br /> <br />4-6- <br /> <br />/ <br />/ <br />/ <br /> <br />'\ 4' <br /> <br /><4' <br /> <br />Buffalo <br />Creek <br />x <br /> <br /><4" <br /> <br />o <br /> <br />10 <br /> <br /> <br />1. Location of paleoflood study for eastern Colorado. Basin boundaries are shown for the larger <br />basins draining from the Palmer Divide. Maximum 24-hour rainfall isohyets for large <br />rainstorms in the study area (modified from Hansen and others, 1978) also are shown. <br />Maximum rainfall amounts are centered on isolated buttes and ridges, which exacerbate rainfall <br />amounts. <br />