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Science 19 March 1982:
Vol. 215. no. 4539, pp. 1463 - 1468
DOI: 10.1126/science.215.4539.1463

Articles

The Columbia River Basalts

Peter R. Hooper 1

1 Professor of geology, Washington State University, Pullman 99164

Between 17 million and 6 million years ago, 200,000 square kilometers of the American Northwest were flooded by basaltic lava that erupted through fissures in the crust up to 150 kilometers long. Larger individual eruptions covered over a third of the Columbia Plateau in a few days. The lavas represent partial melts of the earth's mantle that were only slightly modified by near-surface, upper crustal processes. The abundant chemical and mineralogical data now available offer an opportunity to study mantle composition and the processes involved in the evolution of the earth's crust.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Geochemical Controls on Contaminant Uranium in Vadose Hanford Formation Sediments at the 200 Area and 300 Area, Hanford Site, Washington.
J. P. McKinley, J. M. Zachara, J. Wan, D. E. McCready, and S. M. Heald (2007)
Vadose Zone J. 6, 1004-1017
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Rare earth element geochemistry of groundwater in the Palouse Basin, northern Idaho-eastern Washington.
B. J. Nelson, B. J. Nelson, S. A. Wood, and J. L. Osiensky (2004)
Geochemistry: Exploration, Environment, Analysis 4, 227-241
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Preeruption history of the Grande Ronde Formation lavas, Columbia River Basalt Group, American Northwest: Evidence from phenocrysts.
S. R. Durand and G. Sen (2004)
Geology 32, 293-296
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The eruption environment of multi-tiered columnar basalt lava flows.
P. LYLE (2000)
Journal of the Geological Society 157, 715-722
   Abstract »    Full Text »    PDF »
Parana magmatism and the opening of the South Atlantic.
C. J. Hawkesworth, K. Gallagher, S. Kelley, M. Mantovani, D. W. Peate, M. Regelous, and N. W. Rogers (1992)
Geological Society, London, Special Publications 68, 221-240
   Abstract »    PDF »
Flood Basalt Volcanism During the Past 250 Million Years.
M. R. Rampino, M. R. Rampino, and R. B. Stothers (1988)
Science 241, 663-668
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