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<br />E60 <br /> <br />FLOODS OF 1'965 IN THE UNITED STATES <br /> <br />SUMMARY OF FLOODS <br /> <br />Eo1 <br /> <br />30. <br />>5' <br /> <br /> <br />102045' <br /> <br />FLOOD OF JUNE 15 IN THE YELLOWSTONE RIVER BASIN NEAR <br />GLENDIVE, MONT, <br />By-MELVIN V. JOHNSON <br /> <br />~ <br /> <br />Local raIns of high intensities caused severe flooding in a sparsely <br />settled area northeast of Glendive, Mont. (fig. 26) . Weather Bureau in- <br />.formation from unofficial gages shows that precipitation for the storm <br />area ranged from 3.5 to 13,5 inches, A rancher wha lives about 1 mile <br />upstream from che flood-determination point an Griffith Creek stated <br />."Seven inches of rain fell in about half an hour." Precipimtion at the <br />Weather Bureau station 'at Glendive on June 15 was only 0.56 inches. <br /> <br />~ <br />Are~o~re~ <br /> <br />2 0 2 4 <br />I, I I I <br /> <br />MILES EXPLANATION <br />6 -4- <br />I Isoliyet, showing precipitation, <br />in inches <br /> <br />104040' <br /> <br />30' <br /> <br />104"20' <br /> <br />Drainage divide <br /> <br />EXPLANATION <br />. <br />Flood-determination point <br /> <br /> <br />'1 <br />'" <br /> <br />Flood-determination point <br /> <br />FIGURE.25.-Loeation of flood-determination points and isobyets for June 10--11, <br />floods of June 11 in Sanderson Canyon, Tex. Isohyets from U.S. Army Corps of <br />Engineers (unpU!b. data). <br /> <br />Three Mile Draw was 22,400 cfs, and the peak discharge from a 151- <br />sq-mi basin on. Sanderson Canyon was 76,400 cfs. Although Three <br />Mile praw peaked slightly earlier than Sanderson Canyon, the peak <br />discharge through Sanderson was about equal to the sum of the two <br />peaks, about 100,000 cfs. This, the maximum knawn flood at Sander- <br />S\>ll, greatly exceeded the previaus maximum known discharge, cov- <br />ered the valley floor, and inundated about 230 acres of the community. <br />Longtime residents stated that the greatest flood previously known, <br />in 1935, slightly exceeded the channel capacity (about 20,000 cfs) , The <br />statistical probability that a flood of similar magnitude will reoccur <br />in Sanderson is very small because the peak disCharges an Three Mile <br />Praw and on Sanderson Canyon, respectively, were about 4.1 and 5.4 <br />times that of a 50-year flood. <br />At least 24 persons were killed. Acbout 85 persons were injured, 10 <br />of whom were hospitalized, Property damage consisted of destruction <br />of '54 houses and 13 trailer houses; majar damage to 36 houses, 8 trailer <br />houses, and 27 businesses; and minor dam"-ge to 106 houses. Three <br />bridges 'Of the Southern Pacific Lines were destroyed, and more than <br />20 miles of U.S. Highway 90 was damaged. Pamage in Sanderson <br />(estimated 1965 popnlation, 2,189) and vicinity was estimated at <br />$2,664,000. <br /> <br />47"10' <br /> <br /> <br />47"00' <br /> <br />o <br />I <br /> <br />SMILES <br />I <br /> <br />FIGURE 26.-Location of flood-determination point. :flood of June 15 near <br />Glendive, Mont. <br />