GLACIAL LAKE MISSOULA
(Redirected from Lake Missoula)
'Glacial Lake Missoula' was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago. The lake measured about and contained about of water, half the volume of Lake Michigan.[1]
The lake was the result of an ice dam on the Clark Fork River caused by the southern encroachment of a finger of the Cordilleran Ice Sheet into the Idaho Panhandle (at the present day location of Lake Pend Oreille). The height of the ice dam typically approached , flooding the valleys of western Montana approximately eastward. It was the largest ice-dammed lake known to have occurred. Northwest Exposures: A Geologic History of the Northwest, , David, Alt, Mountain Press, , ISBN 0-87842-323-0
The periodic rupturing of the ice dam resulted in the Missoula Floods--cataclysmic floods that swept across Eastern Washington and down the Columbia River Gorge approximately 40 times during a 2,000 year period. The cumulative effect of the floods was to excavate of loess, sediment and basalt from the channeled scablands of eastern Washington and to transport it downstream. Cataclysms on the Columbia : a layman's guide to the features produced by the catastrophic Bretz floods in the Pacific Northwest, , John Eliot, Allen, Timber Press, , ISBN 0881920673 These floods are noteworthy for producing canyons and other large geologic features through cataclysms rather than through gradual processes.
★ Glacial lake outburst flood
★ List of prehistoric lakes
1. On the trail of the Ice Age floods : a geological field guide to the mid-Columbia basin / Bruce Bjornstad., , Bruce N., Bjornstad, Keokee Books, , ISBN 9781879628274
★ USGS Site on Glacial Lake Missoula
★ PBS's NOVA (TV series): Mystery of the Megaflood for information on the Missoula Floods
'Glacial Lake Missoula' was a prehistoric proglacial lake in western Montana that existed periodically at the end of the last ice age between 15,000 and 13,000 years ago. The lake measured about and contained about of water, half the volume of Lake Michigan.[1]
The lake was the result of an ice dam on the Clark Fork River caused by the southern encroachment of a finger of the Cordilleran Ice Sheet into the Idaho Panhandle (at the present day location of Lake Pend Oreille). The height of the ice dam typically approached , flooding the valleys of western Montana approximately eastward. It was the largest ice-dammed lake known to have occurred. Northwest Exposures: A Geologic History of the Northwest, , David, Alt, Mountain Press, , ISBN 0-87842-323-0
The periodic rupturing of the ice dam resulted in the Missoula Floods--cataclysmic floods that swept across Eastern Washington and down the Columbia River Gorge approximately 40 times during a 2,000 year period. The cumulative effect of the floods was to excavate of loess, sediment and basalt from the channeled scablands of eastern Washington and to transport it downstream. Cataclysms on the Columbia : a layman's guide to the features produced by the catastrophic Bretz floods in the Pacific Northwest, , John Eliot, Allen, Timber Press, , ISBN 0881920673 These floods are noteworthy for producing canyons and other large geologic features through cataclysms rather than through gradual processes.
| Contents |
| See also |
| Cited references |
| External links |
See also
★ Glacial lake outburst flood
★ List of prehistoric lakes
Cited references
1. On the trail of the Ice Age floods : a geological field guide to the mid-Columbia basin / Bruce Bjornstad., , Bruce N., Bjornstad, Keokee Books, , ISBN 9781879628274
External links
★ USGS Site on Glacial Lake Missoula
★ PBS's NOVA (TV series): Mystery of the Megaflood for information on the Missoula Floods
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