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Lake Condon information


Lake Condon
Historical location of Lake Condon in Oregon
Historical location of Lake Condon in Oregon
Lake Condon
Lake Condon's historical location in Oregon, USA
LocationNorth America
Coordinates45°55′09″N 119°21′20″W / 45.919167°N 119.355556°W / 45.919167; -119.355556
Lake typeformer lake
Primary inflowsWallula Gap of the Columbia River
Primary outflowsColumbia River Gorge
Basin countriesUnited States
Max. length110 mi (180 km)
Max. width57 mi (92 km)
Average depth600 ft (183 m)
Max. depth1,000 ft (305 m)
Water volume116 cu mi (480 km3)
Residence time2.6 years
Surface elevation1,000 ft (305 m)
References[1]

Lake Condon was a temporary lake in the Pacific Northwest region of North America, formed periodically by the Missoula Floods from 15,000 to 13,000 BC. It was named after Oregon geologist Thomas Condon.

The restricted flow of waters[2] from cataclysmic floods from Glacial Lake Missoula, and pluvial Lake Bonneville through the constriction of the Wallula Gap in the Horse Heaven Hills flowed into south-central Washington and north-central Oregon, and were backed up by the Columbia River Gorge, forming Lake Condon. The water remained for a period of 5–7 days before the flood waters drained through the Columbia River Gorge. Lake Condon reached an elevation of about 1200 feet above sea level (today's sea level) before subsiding.[3][4][5]

Lake Condon also flooded the Umatilla and John Day river valleys.[6]

  1. ^ "A Guide to the Ice Age Floods in the Columbia River Gorge, Our Cataclysmic Floodscape". www.iafi.org. Ice Age Floods Institute. 21 October 2019. Retrieved 2021-02-20.
  2. ^ Flow was restricted by a hydraulic dam—a restriction to the flow rate caused by a narrowed reach in a river valley.
  3. ^ United States Geological Service Site
  4. ^ "Ice Age Floods Institute site on Lake Lewis". Archived from the original on 2007-01-01. Retrieved 2009-09-12.
  5. ^ 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.
  6. ^ Carson, Robert J.; Pogue, Kevin R. (1996). Flood Basalts and Glacier Floods:Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington. Washington State Department of Natural Resources (Washington Division of Geology and Earth Resources Information Circular 90). ISBN none.

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