Prairie, Peak, and Plateau: A Guide to the Geology of ColoradoChronic, John
Science
Prairie, Peak, and Plateau: A Guide to the Geology of Colorado
Chronic, John
Geology -- Colorado -- Guidebooks
“The morning of June 16 was most pleasant, but conditions changed
rapidly shortly before noon. A tornado touched ground 15 miles south
southeast of Denver about 1 p.m. Within the next hour, another unroofed
30 homes in the little town of Palmer Lake, 40 miles south of Denver.
About 2 p.m., a dense mass of clouds descended and concealed the top of
Dawson Butte, 7 miles southwest of Castle Rock; and the little light
remaining faded until it was dark black and frightening, according to
some people. A nearby rancher’s wife described the intense quiet as
awesome, but the calm did not last very long.
“The deluge began, not only near Dawson Butte, but also at Raspberry
Mountain, 6 miles to the south, near Larkspur. The rain came down harder
than any rain the local residents had ever seen, and the temperature
dropped rapidly until it was cold. The quiet was shattered by the
terrible roar of wind, rain, and rushing water. Then the thudding of
huge boulders, the snapping and tearing of trees, and the grinding of
cobbles and gravel increased the tumult. The small natural channels on
the steep slopes could not carry the runoff; so water took shortcuts,
following the line of least resistance. Creeks overflowed, roads became
rivers, and fields became lakes—all in a matter of minutes.
“The flow from glutted ravines and from fields and hillsides soon
reached East and West Plum Creeks. The combined flow in these creeks
have been described as awesome, fantastic, and unbelievable; yet none of
these superlatives seem adequate to describe what actually occurred.
Large waves, high velocities, crosscurrents, and eddies swept away
trees, houses, bridges, automobiles, heavy construction equipment, and
livestock. All sorts of debris and large volumes of sand and gravel were
torn from the banks and beds of the streams and were dumped, caught,
plastered, or buried along the channel and flood plains downstream. A
local resident stated, ‘The banks of the creek disappeared as if the
land was made of sugar.’
“The flood reached the South Platte River and the urban areas of
Littleton, Englewood, and Denver about 8 p.m. Here the rampaging waters
picked up house trailers, large butane storage tanks, lumber, and other
flotsam and smashed them against bridges and structures near the river.
Many of the partly plugged bridges could not withstand the added
pressure and washed out. Other bridges held, but they forced water over
approach fills, causing extensive erosion. The flood plains carried and
stored much of the flood water, which inundated many homes, businesses,
industries, railroad yards, highways, and streets.
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