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・ Channel Zero (company)
・ Channel, California
・ Channel-associated signaling
・ Channel-billed cuckoo
・ Channel-billed toucan
・ Channel-conductance-controlling ATPase
・ Channel-inducing factor 4
・ Channel-iron deposits
・ Channel-Port aux Basques
・ Channel-state duality
・ Channel-stopper
・ Channel-to-channel adapter
・ ChannelAdvisor
・ ChannelBee
・ Channeled pebblesnail
Channeled Scablands
・ Channeled whelk
・ ChannelFlip
・ ChannelGain
・ Channeling
・ Channeling the Quintessence of Satan
・ Channelization
・ Channelization (roads)
・ Channelization (telecommunications)
・ Channell
・ Channelling (physics)
・ Channelling Baby
・ Channellock
・ Channelome
・ Channelopathy


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Channeled Scablands : ウィキペディア英語版
Channeled Scablands

The Channeled Scablands are a relatively barren and soil-free landscape on the eastern side of the U.S. state of Washington that was scoured by floods unleashed when a large glacial lake drained.〔Marshak, Stephen, 2009, ''Essentials of Geology,'' W. W. Norton & Company, 3rd ed. ISBN 978-0393196566〕 These cataclysmic Missoula Floods swept periodically across eastern Washington and down the Columbia River Plateau during the Pleistocene epoch. Geologist J Harlen Bretz coined the term "channeled scablands" in a series of papers written in the 1920s. The debate on the origin of the Scablands that ensued for four decades became one of the great controversies in the history of earth science. The Scablands are also important to planetary scientists as perhaps the best terrestrial analog of the Martian outflow channels.〔Carr, M. H. (2006), ''The Surface of Mars''. Cambridge Planetary Science Series, Cambridge University Press.〕
==History==
Bretz conducted research and published many papers during the 1920s describing the Channeled Scablands. His theories of how they were formed required short but immense floods (500 cubic miles of water), for which Bretz had no explanation. Bretz's theories met with vehement opposition from geologists of the day, who tried to explain the features with uniformitarian theories.
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 Missoula Floods and creator of the Channeled Scablands.
Pardee's and Bretz's theories were accepted only after decades of painstaking work and fierce scientific debate. Research on open channel hydraulics in the 1970s put Bretz's theories on solid scientific ground. In 1979 Bretz received the highest medal of the Geological Society of America, the Penrose Medal, to recognize that he had developed one of the great ideas in the earth sciences.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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