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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 7,770 square kilometres (3,000 sq mi) and contained about 2,100 cubic kilometres (500 cu mi) of water, half the volume of Lake Michigan .
Alt, David (2001) Glacial Lake Missoula and Its Humongous Floods (Mountain Press, 2001. ISBN 978-0878424153). Norman B. Smyers and Roy M. Breckenridge (2003). "Glacial Lake Missoula, Clark Fork ice dam, and the floods outburst area: Northern Idaho and western Montana". In T. W. Swanson (ed.). Western Cordillera and adjacent areas. Geological ...
The Ice Age Floods National Geologic Trail is a network of routes connecting natural sites and facilities that provide interpretation of the geological consequences of the Glacial Lake Missoula floods of the last glacial period that occurred about 18,000 to 15,000 years ago. It includes sites in Washington, Oregon, Idaho, and Montana.
Glacial Lake Missoula. Between 15,000 and 13,000 years ago, Glacial Lake Missoula formed when an ice sheet blocked the Clark Fork River, damming up the river's water back into the valleys of western Montana. [5] The dam would periodically burst causing a flood of water to rush across Idaho, Washington and Oregon to the Pacific Ocean.
The history of Missoula, Montana begins as early as 12,000 years ago with the end of the region's glacial lake period with western exploration dating back to the Lewis and Clark Expedition of 1804–1806. The first permanent settlement was founded in 1860.
Medicine Lake Site: 1980: Sheridan: federal (Medicine Lake National Wildlife Refuge) An exceptional example of the processes of continental glaciation, including till, outwash, eskers, kames, and terrace deposits.
Giant current ripples are an important feature of the Channeled Scablands in Washington state, U.S., which formed during the Last Glacial Maximum as a result of at least 39 glacial lake bursts, called the Missoula floods, which originated from glacial lakes Columbia in Washington and Missoula in Montana. [10] [11] [12] [13]
J. T. Pardee first suggested in 1925 to Bretz that the draining of a glacial lake could account for flows of the magnitude needed. Pardee continued his research over the next 30 years, collecting and analyzing evidence that eventually identified Lake Missoula as the source of the floods (now the Missoula floods) and creator of the Channeled ...