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<br /> <br />40 <br /> <br />20 <br /> <br /> <br />Scoured colluvium <br /> <br /> <br />I Range of 1933 <br />fl~Od level = PSI <br /> <br />------------------- ---- <br /> <br />Dol. 't.", <br /> <br />.....1..,......,4. <br /> <br />.... <br />- <br /> <br />30 <br /> <br />Boulders <br /> <br />- <br />c:: <br />o <br /> <br />Colluvium <br /> <br />.... <br />C'Cl <br />> <br /><ll <br />W <br /> <br />10 <br /> <br />. <br />1933 " <br />Flood bar ,,' <br />............---..- <br /> <br />slope = 0.032 fllft <br /> <br />o <br />o <br /> <br />100 200 <br />Stationing, ft <br /> <br />300 <br /> <br />400 <br /> <br />2, Cherry Creek near Franktown streamflow-gaging station (0671200), which is located <br />about 2,5 miles south of Franktown: a.) Photograph showing downstream view of paleoflood <br />reach and 1933 dam-failure flood deposits (PSI) with rod held level with the top of PSis for <br />cross section located about 500 feet downstream from the gage; and b,) graph of channel cross <br />section, The highest paleostage indicator is constrained by un eroded. old colluvium and a f100d- <br />deposited boulder bar (-700 x 300 x > 1 0 feet) deposited by the 1933 dam-failure flood, The <br />largest surface boulders are more than 6 feet in diameter; 1933 flood-transported boulders <br />more than 25 feet in diameter are located upstream and downstream from this paleoflood site, <br />The range of peak discharge is 30,000 to 44,000 fl3/s, <br /> <br />I <br />