Laserfiche WebLink
<br />, <br /> <br />,. <br /> <br />. <br /> <br />50 <br /> <br />FLOODS IN COLORADO <br /> <br />June 7-10, 1923, heavy rains occurrcd June 14-16 ovcr an area ex- <br />tending from a point a few miles east of Greeley to the western edge <br />of R. 70 W. in the foothills rcgion, and appeared to center over the <br />lower part of Buckhorn Creek Basin. The resulting flood, the high- <br />est known on Buckhorn Creek and several of its tributaries, was <br />investigated within a few days by the Geological Survey, and the <br />. ,( results were published." The area affected extended from the mouth <br />V' of Buckhorn Creek to a point 5 milcs above Masonville and a short <br />distance above the mouth of Missouri Canyon. A 30-minute rainfall <br />of 2~ inches was mcasured in a tub. <br />The following table shows the peak discharge at the three points <br />measured: <br /> <br />Peak discharge in Buckhorn Creek Basin, June 15, 19~3 <br /> <br /> Drainage area Peak discharge <br /> (SQuaN.lIlliles) <br /> Second- 'l'imeof <br />s"",,no Location Area. root per flool1 <br /> Total pro- Second- square crest <br /> dncing feet mUcor <br /> .ood Bl'CaM- <br /> rected <br /> - <br />Duckhorn Creek____ Haifa mllesoutb or M8soDvllle._. 1M 40 10,500 262 tOp.tn. <br />Redstone Creek.un MasonvillIL________.._. ...._______ 31 21 6,820 325 lOp. Ill. <br />Missouri Canyon.._ NlW' mouth, sec. 26, T. 6 N., R. 2.' 2.' 4.,350 1,810 6::lUp. Ill. <br /> 70W. <br /> <br />A peak discharge of almost equal amount occurred on Buckhorn <br />Creek following the storm of September I, 1938, in the foothills arca. <br />o The area of precipitation did not extend more than 2 miles above <br />Masonville on the main stream, but in the tributary basin of Red- <br />stone Creek, the storm extended practically to the head of the basiu" <br />A slope-area measurement of the flood on Redstone Creek, which <br />occurred at 10 p. m. Scptember 1, was made a quarter of a mile above <br />its mouth, and the peak discharge was determined at 8,400 sccond- <br />feet, or 271 second-feet per square mile from a drainage area of 31 <br />square miles, The peal< discharge of Buckhorn Creek at a point 2~ <br />miles below :tI1asonville was 10,200 second-feet, or 196 second-feet per <br />square mile from the 52 square miles affected by the storm. The <br />greater part of this flow was absorbed by Buckhorn l\eservoir, which <br />is located a mile below the point of measurement, and has a capacity <br />of 650 acre-feet. <br />During the storm of September 10, 1938, a cloudburst centered over <br />?./ Missouri Canyon. A rancher living in sec. 23, T. 6 N., R. 70 W., <br />1~ miles above the mouth of Missouri Canyon, measured in a straight- <br />sided can a rainfall of about 5 inches, which occurred between 6 and <br /> <br />II Follansbee, Robert, and Hodges. P. v" Borne floods In the Rocky Mountain region; U. 8. Geol. Sur- <br /> <br />T <br /> <br />MAJOR FLOOnS--SOUTH PLATTE RIVER <br /> <br />51 <br /> <br />7 p. m., September 10, most of it within 20 minutes. Another rancher <br />who lives 1 mile above the mouth of Missouri Canyon measured in a <br />straight-sided can about 7 inchcs of rain which fell within half an hour. <br />Half a mile south, a rainfall of 2~ inches was reported. A slope-area <br />measurement of the flow of Missouri Canyon in sec. 26, T. 6 N., l\. <br />70 W., showed a peak discharge of 2,130 second-feet from a drainage <br />area of 2.37 square miles, or 899 second-feet per square mile. <br /> <br />CACHE LA PQUDRE RIVER <br /> <br />Above B?llvue the Cache la Poudre l\iver drains the Front Range, <br />and for a dIStance of 13 miles above the gaging station at the mouth <br />of the canyon the fall is 63 feet per mile. Across the plains from the <br />mouth of the canyon to the mouth of the river, a distance of 41 miles, <br />the fnll is 16 feet per mile. <br /> <br />Gaging stations in Cache la Poudre River Basin <br /> <br />Station <br /> <br />nraina.~p. area <br />(squaromilcs) <br /> <br />Pcriodofrooord <br /> <br />North Jo'ork Cache In Poudre River at . <br />Y.lvermorc. <br />. Cnchc In }'ol1drc River at mouth of canyon <br />near Fort Collins. ' <br />Cache la Poudre River neDr OreeleYuhu.H <br /> <br />May ID29 to Beptemoor 1931. <br />March 1884 to date (carller years fmgmen. <br />tary). <br />March 1903 to November 1004; February 191. <br />to DCtxlUlOOr 1919; May 1924 to date. <br /> <br />Ml <br />1.... <br />1,840 <br /> <br />In connection with meager evidence of a widespread flood in 1844, <br />Watrous" quotes a letter from Antoine Janis, a French trapper who <br />was living on the river near the present town of Laporte: . <br /> <br />On the first of June, 1844, I stuck my stake on a claim in the valley. * * * <br />At that time the streams were all very high and the Valley black with buffalo. <br /> <br />In the same volume Watrous refers to a flood in 1864: <br /> <br />Fort Collins} the county Beat and principal town in Larimer County, owes its <br />origin and first place on the map to the intervention of a flood in the Cache 1& <br />Poudre River. This flood occurecl on the last days of May and first davs of June <br />1864 and is said to have been the worst known by white men. The water poured <br />out of the banks of the stream and inundated the valley from bluff to bluff with <br />a torrent, that carried everything not firmly attached to the soil with it. <br />It carried O\lt the toll bridge at Laporte at a time when the movement of emi- <br />gration westward was the heaviest, and more than 200 emigrants were stalled on <br />the bluffs south of Laporte} being unable to ford the stream because of high <br />water. * * * <br />In the spring of 1864, under the influence of the sun's warm rays, the great <br />masses of snow melted on the hillsides and torrents of water came pouring down <br />fr?m ~hc slopes into the channel of the Cache 18 Poudre, swelling the stream even <br />With Ita banks. On the 9th of June, an extraordinary rainstorm set in on the <br />watershed of the upper part of the river, melted the Bnow in the higher altitudes 1/ <br /> <br />" Watrous, Ansel} History of Larimer County: Conner Printing & PUblishing Co. Fort Colllas Cot... <br />1911. .' . <br />