Channeled Scabland
Este artigo ou secção contém uma lista de referências no fim do texto, mas as suas fontes não são claras porque não são citadas no corpo do artigo, o que compromete a confiabilidade das informações. (setembro de 2020) |

O Channeled Scabland é um deserto localizado em Washington, nos Estados Unidos. Ele foi criado pelas inundações de Missoula, uma série de eventos cataclísmicos de explosão de lagos glaciais que varreram periodicamente o leste de Washington e desceram o desfiladeiro do rio Columbia no final da última era glacial.
O Rio Vales forma vales e cânions em forma de "V" ao longo do deserto.
Referências Bibliográficas
- Bretz, J Harlen (1923), "The Channeled Scabland of the Columbia Plateau." Journal of Geology, v.31, p.617-649.
- Bretz, J Harlen (1925), "The Spokane flood beyond the Channeled Scablands." Journal of Geology, v.33, p.97-115, 236-259.
- Bretz, J H.; Smith, H.T.U.; and Neff, G.E., (1956) "Channeled Scabland of Washington — New Data and Interpretations." Geological Society of America Bulletin, v.67, p.957-1049.
- Allen, John Eliot; Marjorie Burns; and Sam C. Sargent. (1986) Cataclysms on the Columbia. Portland, Oregon: Timber Press, ISBN 0-88192-215-3
- Soennichsen, John (2008), "Bretz's Flood: The Remarkable Story of a Rebel Geologist and the World's Greatest Flood", Seattle, Washington, Sasquatch Books, ISBN 978-1-57061-505-4
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