The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin
The Channeled Scabland of eastern Washington State, USA, brought megafloods to the scientific forefront. A 30,000-km2 landscape of coulees and cataracts carved into the region’s loess-covered basalt attests to overwhelming volumes of energetic water. The scarred landscape, garnished by huge boulder...
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Online Access: | https://archimer.ifremer.fr/doc/00624/73634/73074.pdf https://doi.org/10.1016/j.earscirev.2020.103181 https://archimer.ifremer.fr/doc/00624/73634/ |
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ftarchimer:oai:archimer.ifremer.fr:73634 2023-05-15T16:40:47+02:00 The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin O’connor, Jim E. Baker, Victor R. Waitt, Richard B. Smith, Larry N. Cannon, Charles M. George, David L. Denlinger, Roger P. 2020-09 application/pdf https://archimer.ifremer.fr/doc/00624/73634/73074.pdf https://doi.org/10.1016/j.earscirev.2020.103181 https://archimer.ifremer.fr/doc/00624/73634/ eng eng Elsevier BV https://archimer.ifremer.fr/doc/00624/73634/73074.pdf doi:10.1016/j.earscirev.2020.103181 https://archimer.ifremer.fr/doc/00624/73634/ info:eu-repo/semantics/openAccess restricted use Earth-science Reviews (0012-8252) (Elsevier BV), 2020-09 , Vol. 208 , P. 103181 (51p.) Megafloods Columbia River basin western North America Missoula floods Bonneville flood Channeled Scabland text Publication info:eu-repo/semantics/article 2020 ftarchimer https://doi.org/10.1016/j.earscirev.2020.103181 2023-03-14T23:55:18Z The Channeled Scabland of eastern Washington State, USA, brought megafloods to the scientific forefront. A 30,000-km2 landscape of coulees and cataracts carved into the region’s loess-covered basalt attests to overwhelming volumes of energetic water. The scarred landscape, garnished by huge boulder bars and far-travelled ice-rafted erratics, spurred J Harlen Bretz’s vigorously disputed flood hypothesis in the 1920s. First known as the Spokane flood, it was rebranded the Missoula flood once understood that the water came from glacial Lake Missoula, formed when the Purcell Trench lobe of the last-glacial Cordilleran ice sheet dammed the Clark Fork valley in northwestern Idaho with ice a kilometer thick. Bretz’s flood evidence in the once-remote Channeled Scabland, widely seen and elaborated by the 1950s, eventually swayed consensus for cataclysmic flooding. Missoula flood questions then turned to some that continue today: how many? when? how big? what routes? what processes? The Missoula floods passed through eastern Washington by a multitude of valleys, coulees and scabland tracts, some contemporaneously, some sequentially. Routings and their timing depended on the positions of various lobes of the multi-pronged Cordilleran ice sheet and the erosional development of the channels themselves. The first floods mostly followed the big bend of Columbia valley looping through north-central Washington. But the south-advancing Okanogan ice lobe soon blocked that path, forming long-lasting glacial Lake Columbia in the impounded Columbia valley. Missoula floods into this lake were diverted south out of the Columbia valley and into eastern Washington coulees and scabland tracts. At least four floods entered Moses Coulee, but then as the Okanogan lobe advanced over and blocked the head of that coulee, more eastern paths took the water, including Grand Coulee and the Telford-Crab-Creek and Cheney-Palouse scabland tracts. Flood routing also depended on the erosion of the coulees. At some point, headward erosion of upper Grand ... Article in Journal/Newspaper Ice Sheet Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Crab Creek ENVELOPE(-57.625,-57.625,-62.019,-62.019) Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Moses ENVELOPE(-99.183,-99.183,-74.550,-74.550) Earth-Science Reviews 208 103181 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Megafloods Columbia River basin western North America Missoula floods Bonneville flood Channeled Scabland |
spellingShingle |
Megafloods Columbia River basin western North America Missoula floods Bonneville flood Channeled Scabland O’connor, Jim E. Baker, Victor R. Waitt, Richard B. Smith, Larry N. Cannon, Charles M. George, David L. Denlinger, Roger P. The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
topic_facet |
Megafloods Columbia River basin western North America Missoula floods Bonneville flood Channeled Scabland |
description |
The Channeled Scabland of eastern Washington State, USA, brought megafloods to the scientific forefront. A 30,000-km2 landscape of coulees and cataracts carved into the region’s loess-covered basalt attests to overwhelming volumes of energetic water. The scarred landscape, garnished by huge boulder bars and far-travelled ice-rafted erratics, spurred J Harlen Bretz’s vigorously disputed flood hypothesis in the 1920s. First known as the Spokane flood, it was rebranded the Missoula flood once understood that the water came from glacial Lake Missoula, formed when the Purcell Trench lobe of the last-glacial Cordilleran ice sheet dammed the Clark Fork valley in northwestern Idaho with ice a kilometer thick. Bretz’s flood evidence in the once-remote Channeled Scabland, widely seen and elaborated by the 1950s, eventually swayed consensus for cataclysmic flooding. Missoula flood questions then turned to some that continue today: how many? when? how big? what routes? what processes? The Missoula floods passed through eastern Washington by a multitude of valleys, coulees and scabland tracts, some contemporaneously, some sequentially. Routings and their timing depended on the positions of various lobes of the multi-pronged Cordilleran ice sheet and the erosional development of the channels themselves. The first floods mostly followed the big bend of Columbia valley looping through north-central Washington. But the south-advancing Okanogan ice lobe soon blocked that path, forming long-lasting glacial Lake Columbia in the impounded Columbia valley. Missoula floods into this lake were diverted south out of the Columbia valley and into eastern Washington coulees and scabland tracts. At least four floods entered Moses Coulee, but then as the Okanogan lobe advanced over and blocked the head of that coulee, more eastern paths took the water, including Grand Coulee and the Telford-Crab-Creek and Cheney-Palouse scabland tracts. Flood routing also depended on the erosion of the coulees. At some point, headward erosion of upper Grand ... |
format |
Article in Journal/Newspaper |
author |
O’connor, Jim E. Baker, Victor R. Waitt, Richard B. Smith, Larry N. Cannon, Charles M. George, David L. Denlinger, Roger P. |
author_facet |
O’connor, Jim E. Baker, Victor R. Waitt, Richard B. Smith, Larry N. Cannon, Charles M. George, David L. Denlinger, Roger P. |
author_sort |
O’connor, Jim E. |
title |
The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
title_short |
The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
title_full |
The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
title_fullStr |
The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
title_full_unstemmed |
The Missoula and Bonneville floods—A review of ice-age megafloods in the Columbia River basin |
title_sort |
missoula and bonneville floods—a review of ice-age megafloods in the columbia river basin |
publisher |
Elsevier BV |
publishDate |
2020 |
url |
https://archimer.ifremer.fr/doc/00624/73634/73074.pdf https://doi.org/10.1016/j.earscirev.2020.103181 https://archimer.ifremer.fr/doc/00624/73634/ |
long_lat |
ENVELOPE(-57.625,-57.625,-62.019,-62.019) ENVELOPE(-129.463,-129.463,58.259,58.259) ENVELOPE(-99.183,-99.183,-74.550,-74.550) |
geographic |
Crab Creek Glacial Lake Moses |
geographic_facet |
Crab Creek Glacial Lake Moses |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Earth-science Reviews (0012-8252) (Elsevier BV), 2020-09 , Vol. 208 , P. 103181 (51p.) |
op_relation |
https://archimer.ifremer.fr/doc/00624/73634/73074.pdf doi:10.1016/j.earscirev.2020.103181 https://archimer.ifremer.fr/doc/00624/73634/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1016/j.earscirev.2020.103181 |
container_title |
Earth-Science Reviews |
container_volume |
208 |
container_start_page |
103181 |
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1766031204051582976 |