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<br />
<br />FLOOD HISTORY
<br />
<br />In 1965, a unique combination of orographic effects and meteo-
<br />rological conditions in the South Platte River Basin caused the
<br />worst flooding in the region's recorded history. Severe thunder-
<br />storms commenced over the headwaters of Plum Creek and Cherry
<br />Creek on June 16, and moved northeasterly down the creeks fol-
<br />lowing and augmenting peak flows. More than 14 inches of rain
<br />was recorded at Palmer Lake in 4 hours. Overnight, westerly
<br />winds moved the storm front to a position over the Kiowa and
<br />Bijou Creek Basins where it met with thunderstorms forming just
<br />south of Agate. Here 5.25 inches fell in 45 minutes. The net
<br />results of these conditions were six persons drowned, two other
<br />deaths caused by flood-related activities, and estimated damages
<br />of $500 million in the South Platte River Basin, of which $300
<br />million occurred in the Denver area. (Ref. 4)
<br />
<br />Major floods in the Adams County area have been observed and
<br />recorded on the South Platte River and its tributaries since
<br />1844. During that period, eleven major floods have occurred.
<br />
<br />In 1844 and 1864, reports stated that "bottom1ands near Den-
<br />ver were covered with water bluff to bluff" (Ref. 5). By
<br />1876, encroachment into the flood plain had developed to
<br />such an extent that on May 23, 1876, the Rocky Mountain News
<br />reported that, "(The South Platte River) was higher to be
<br />sure ... several feet. higher perhaps in 1864 ... but it was
<br />not able to work such destruction at that time as now. There
<br />was not so much town here in 1864, as now, nor as many bridges."
<br />(Ref. 1).
<br />
<br />Floods on the South Platte River have been generated near the
<br />slopes of Monument Divide, a high ridge located between Castle
<br />Rock and Colorado Springs, extending from the Rocky Mountains
<br />down to the plains near Limon, Colorado.
<br />
<br />In 1973, the May snowpack over the South Platte River tributary
<br />basins varied from normal to 170 percent above normal. Early
<br />warmer temperatures at higher elevations caused abnormally high
<br />snowmelt runoff, which was augmented by the prolonged rainfall
<br />of May 5 - 6 to produce the worst flooding on the South Platte
<br />River since June 1965. Urban, rural and transportation flood
<br />damages were estimated at $99,500,000 (Ref. 3). Of these, the
<br />rural - agricultural category registered the greatest amount of
<br />damages, because of the extensive damage to public and private
<br />irrigation works and the widespread loss of crops due to inunda-
<br />tion, erosion, and sedimentation. Massive deposition of sediment
<br />on agricultural lands made it impossible to produce crops for two
<br />years. High water marks observed during this flood are shown on
<br />the drawings and recorded in the F100dway tables in the appendix.
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<br />The most significant floods of recent times on the South Platte
<br />River occurred in 1912, 1921, 1933, 1935, 1942, 1965, and 1973.
<br />The discharges for these floods were 13,000 cubic feet per
<br />second (cfs), 8,790 cfs, 22,000 cfs, 12,320 cfs, 10,200 cfs,
<br />40,300 cfs, and 33,000 cfs, respectively, at the Henderson
<br />gage (located near Henderson, Colorado).
<br />
<br />Past floods have resulted from snowmelt and intensive rain
<br />storms over the mountain tributaries, rainstorms over the
<br />eastern tributaries, and combinations of these conditions.
<br />
<br />Scenes of historic floods in Adams County are shown in Figures 1
<br />through 8.
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