Lake Allison
| Lake Allison | |
|---|---|
| Location | Willamette Valley, Oregon |
| Primary inflows | Glacial Lake Missoula |
| Basin countries | United States |
| Max. length | 111 mi (179 km) |
| Max. width | 31 mi (50 km) |
| Surface area | 3,000 sq mi (7,800 km2)[1] |
| Average depth | 200 ft (61 m)[1] |
| Max. depth | 400 ft (120 m)[1] |
Lake Allison was a temporary lake in the Willamette Valley of Oregon, formed periodically by the Missoula Floods from 15,000 to 13,000 BC. The lake is the main cause for the rich and fertile soil that Willamette Valley is now recognized for.
History
Willamette Valley fertility, like the Palouse silt[1] is in large part due to the largest freshwater flood scientifically documented[2] in history. The ice floods started in Lake Missoula in Montana 12,000 to 15,000 years ago during the Pleistocene[3] and flowed down through eastern Washington State, bringing fertile soil to the valley as it flowed out Columbia River Gorge. The narrows at Kalama, Washington restricted the flow of water, causing it to back up, flooding the Willamette Valley to a depth of 300 or 400 feet above sea level, and reached as far as Eugene, Oregon.[2][4][5][6] The Willamette Valley had multiple floods during the last ice age, possibly reaching 100 floods separated by centuries,[2] to depths of 300–400 feet.[6][7] If 300–400 foot-deep floodwaters descended on the Valley today, in Portland (elevation 20 ft), only the tops of the West Hills, Mount Tabor, Rocky Butte, Kelly Butte and Mount Scott would be visible,[7] as would the US Bancorp Tower (536 feet) and the Wells Fargo Center (546 ft). Newberg’s elevation is 175 feet above sea level, Oregon City (138 ft), McMinnville (157 ft), Salem (154 ft), Corvallis (235 ft) and Eugene (430 ft), likely rising above all of them. The lake eventually flowed out and drained, leaving 180 – 200 feet of layered sedimentary soils throughout the Tualatin, Yamhill and Willamette valleys.[1][7]
Name
Geologists named the lake after Oregon State University geologist Ira S. Allison. Among other things, he was the first person to identify and correlate Willamette silt soil in 1953 with soils at the former lakebed of Lake Lewis in Eastern Washington. Ira Allison also documented hundreds of non-native boulders (also known as glacial erratics), in the 1930s, which were transported down the river by the floods on icebergs and left a ring around the lower hills surrounding the Willamette Valley. The most notable of these is the Bellevue Erratic, off Highway 18, west of McMinnville.[6]
See also
References
- ↑ 1.0 1.1 1.2 1.3 1.4 http://www.columbiariverimages.com/Regions/Places/missoula_floods.html
- ↑ 2.0 2.1 2.2 http://www.waymarking.com/waymarks/WM19FR
- ↑ http://depts.clackamas.cc.or.us/science/physci/geology/G145/lectures/wil%20valley.htm
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
- ↑ 6.0 6.1 6.2 Cataclysms on the Columbia, by John Elliott Allen and Marjorie Burns with Sam C. Sargent, 1986. Pages 175-189
- ↑ 7.0 7.1 7.2 Geology of Oregon, by Elizabeth L. Orr, William N. Orr and Ewart M. Baldwin, 1964. Pages 211-214
External links
| Ice Age Glacial Floods |
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| Glacial Lakes | ||
| Temporary Lakes |
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| Ice Age Floods Glacial Residue | ||
| Ice Age Floods Erosion & Deposition Features | ||
| Related contemporaneous events | ||
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