Dry Falls
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In central Washington, on the opposite side of the Grand Coulee from the Columbia River, resides a three and a half mile crescent-shaped precipice known as Dry Falls. Ten times the size of Niagara, Dry Falls is thought to be the greatest known waterfall that ever existed. Geologists speculate that during the last ice age catastrophic flooding channeled water at 65 miles per hour through the Grand Coulee and over this 400-foot rock face. At this time, it is estimated that the flow of the falls was ten times greater than the current flow of all the rivers in the world combined. (Coordinates: )
Nearly twenty thousand years ago, as glaciers moved south, one ice sheet plugged the Clark Fork of the Columbia River, which kept water from being drained from Montana. Consequently a significant portion of western Montana flooded forming the gigantic Lake Missoula. Eventually, enough pressure accumulated on the ice dam that it gave way. It is generally accepted that this process of ice-damming of the Clark Fork, refilling of Lake Missoula and subsequent cataclysmic flooding happened dozens of times over the years of the last Ice Age.[1][2]
This sudden release put parts of Idaho, Washington, and Oregon under hundreds of feet of water in just a few days. These floods, which some consider to be one of the most extraordinary known to man, created the Grand Coulee and Dry Falls in a short period. Similar glacial flooding, though not as impressive as the fore mentioned, kept the falls flowing for the several thousand years.
Once the ice sheets that obstructed the Columbia melted, the river returned to its normal course leaving the Grand Coulee and the falls desiccated. Today, this massive cliff can be viewed from the Dry Falls Interpretive Center, a state park located on Route 17 near the town of Coulee City. Admission is free.
[edit] References
- ^ Alt, David (2001). Glacial Lake Missoula & its Humongous Floods. Mountain Press Publishing Company. ISBN 0-87842-415-6.
- ^ Bjornstad, Bruce (2006). On the Trail of the Ice Age Floods: A Geological Guide to the Mid-Columbia Basin. Keokee Books; San Point, Idaho. ISBN 978-1-879628-27-4.
Allen, John Eliot; Burns, Majorie; and Sargent, Sam C. (1986). Cataclysms on the Columbia. Portland: Timber Press. ISBN 0-88192-215-3.
[edit] External links
| Glacial Lake Missoula | Missoula Floods | Channeled scablands | Grand Coulee | Dry Falls | Drumheller Channels | Columbia River Plateau | Wallula Gap | Touchet Formation | Lake Lewis | Columbia River Gorge | Columbia River Basalt Group | Palouse Falls | Sims Corner Eskers and Kames | Moses Coulee | Withrow Moraine | Crab Creek | Corfu Slide