Lake Great Falls was a prehistoricproglacial lake which existed in what is now centralMontana in the United States between 15,000BCE and 11,000 BCE.[3][4][5] Centered on the modern city ofGreat Falls, Montana, Glacial Lake Great Falls extended as far north asCut Bank, Montana, and as far south asHolter Lake.[6] At present-day Great Falls, the Glacial Lake Great Falls reached a depth of 600 feet (183 metres).[7]
About 13,000 BCE, as the glacier retreated, Glacial Lake Great Falls emptied catastrophically in aglacial lake outburst flood.[5] The meltwater poured through theHighwood Mountains and eroded the hundred mile-long, 500-foot-deep (150 m)Shonkin Sag—one of the most famous prehistoric meltwater channels in the world.[10]
Alden, W. C., 1958, Physiography And Glacial Geology Of Eastern Montana And Adjacent Areas, U. S. Geological Survey Professional Paper 174.
Colton, R. B., Lemke, R. W., and Lindvall, R. M., 1961, Glacial map of Montana East of the Rocky Mountains, U. S. Geological Survey Miscellaneous Geological Investigations Map I-327.
Lindvall, R. M., 1962, Geology Of The Eagle Buttes Quadrangle, Chouteau County, Montana, U. S. Geological Survey Miscellaneous Geological Investigations Map I-349.
Thornbury, W. D., 1965, Regional Geomorphology Of The United States, John Wiley & Sons, Inc., New York.
^Physiography and Glacial Geology of Eastern Montana and Adjacent Areas; William C. Alden; United States Government Printing Office: Washington, D.C.; 1932
^abcMontagne J.L. "Quaternary System, Wisconsin Glaciation."Geologic Atlas of the Rocky Mountain Region. Denver: Rocky Mountain Association of Geologists, 1972.
^abHill, Christopher L. and Valppu, Seppo H. "Geomorphic Relationships and Paleoenvironmental Context of Glaciers, Fluvial Deposits, and Glacial Lake Great Falls, Montana."Current Research in the Pleistocene. 14 (1997); Hill, Christopher L. "Pleistocene Lakes Along the Southwest Margin of the Laurentide Ice Sheet."Current Research in the Pleistocene. 17 (2000); Hill, Christopher L. and Feathers, James K. "Glacial Lake Great Falls and the Late-Wisconsin-Episode Laurentide Ice Margin."Current Research in the Pleistocene. 19 (2002);Reynolds, Mitchell W. and Brandt, Theodore R.Geologic Map of the Canyon Ferry Dam 30' x 60' Quadrangle, West-Central Montana: U.S. Geological Survey Scientific Investigations Map 2860, scale 1:100,000. Scientific Investigations Map 2860. Washington, D.C.: U.S. Geologic Survey, 2005.
^Alt, David and Hyndman, Donald W.Roadside Geology of Montana. Missoula, Mont.: Mountain Press Publishing, 1986.ISBN0-87842-202-1; Stickney, Michael C. "Quaternary Geology and Faulting in the Helena Valley." In1987 Guidebook for the Helena Area, West-Central Montana: Guidebook for the 12th Annual Field Conference. Richard B. Berg and Ray H. Breuninger, eds. Montana Bureau of Mines and Geology Special Publication 95. Helena, Mont.: Montana Bureau of Mines and Geology, 1987.
^abClawson, Roger and Shandera, Katherine A.Billings: The City and the People. Helena, Mont.: Farcountry Press, 1998.ISBN1-56037-037-8
^Axline, Jon and Bradshaw, Glenda Clay.Montana's Historical Highway Markers. Rev. ed. Helena, Mont.: Montana Historical Society, 2008.ISBN0-9759196-4-4; Bowman, Isaiah. "Forest Physiography: Physiography of the United States and Principles of Soils in Relation to Forestry."American Environmental Studies. Reprint ed. Charles Gregg, ed. New York: Arno Press, 1970.ISBN0-405-02659-5
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