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Age of the Last Major Scabland Flood of the Columbia Plateau in Eastern Washington

Published online by Cambridge University Press:  20 January 2017

Donal R. Mullineaux ,
Ray E. Wilcox ,
Walter F. Ebaugh ,
Roald Fryxell  and
Meyer Rubin
Donal R. Mullineaux
Affiliation:
U. S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225 USA and U. S. Geological Survey National Center, Reston, Virginia 22092 USA
Ray E. Wilcox
Affiliation:
U. S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225 USA and U. S. Geological Survey National Center, Reston, Virginia 22092 USA
Walter F. Ebaugh
Affiliation:
U. S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225 USA and U. S. Geological Survey National Center, Reston, Virginia 22092 USA
Roald Fryxell
Affiliation:
U. S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225 USA and U. S. Geological Survey National Center, Reston, Virginia 22092 USA
Meyer Rubin
Affiliation:
U. S. Geological Survey, Box 25046, Federal Center, Denver, Colorado 80225 USA and U. S. Geological Survey National Center, Reston, Virginia 22092 USA
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Abstract

Pumice layers of set S from Mount St. Helens can be correlated with certain ash beds associated with young flood deposits of the channeled scabland. The correlation points to an age of about 13,000 14C yr B.P. for the last major flood to have crossed the scabland. Until recently, the last major episode of flooding was thought to be closer to 20,000 yr B.P., an age inferred chiefly from the relation of the flood to glacial events of the northern Rocky Mountains. Several investigations within the last few years have suggested that the last major flood occurred well after 20,000 yr B.P. Tentative correlations of ash beds of the scabland with set S pumice layers, the relations of flood and glacial events along the northwestern margin of the Columbia Plateau, and a radiocarbon date from the Snake River drainage southeast of the plateau all indicate an age much younger than 20,000 yr. The postulated age of about 13,000 yr B.P. is further supported by a radiocarbon date in the Columbia River valley downstream from the scabland tract. Basal peat from a bog on the Portland delta of Bretz, which is a downvalley deposit of the last major scabland flood, has been dated as 13,080 ± 300 yr B.P. (W-3404).

Type
Original Articles
Information
Quaternary Research , Volume 10 , Issue 2 , September 1978 , pp. 171 - 180
Copyright
University of Washington

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References

Baker, 150.R., 1973. Paleohydrology and sedimentology of Lake Missoula flooding in eastern Washington. Geological Society of America, Special Paper No. 144. 79.Google Scholar
Baker, 151.R., Patton, P.C., 1976. Missoula flooding in the Cheney-Palouse scabland tract. Geological Society of America Abstracts with Programs. 8, No. 3 351-352.Google Scholar
Bretz, JH., 1923. The channeled scablands of the Columbia Plateau. Journal of Geology. 31, 617-649.Google Scholar
Bretz, JH., 1925. The Spokane flood beyond the channeled scablands, 2. Journal of Geology. 33, 236-259.Google Scholar
Bretz, JH., 1929. Valley deposits immediately east of the channeled scabland of Washington, 1. Journal of Geology. 37, 393-427.CrossRefGoogle Scholar
Bretz, JH., 1969. The Lake Missoula floods and the channeled scabland. Journal of Geology. 77, 505-543.Google Scholar
Bretz, JH., Smith, H.T.U., Neff, G.E., 1956. Channeled scabland of Washington—new data and interpretations. Geological Society of America. 67, 957-1050.Google Scholar
Brown, R.E., 1973. The Glacial Lake Missoula floods in the Pasco Basin. Northwest Science Abstract 46th Annual Meeting. Walla Walla, Wash., March 29–31, 1973 6.Google Scholar
Flint, R.F., 1938. Origin of the Cheney-Palouse scabland tract. Geological Society of America Bulletin. 49, 461-523.Google Scholar
Foley, L.L., 1976. Slack water sediments in the Alpowa Creek drainage, Washington. M. A. thesis. Washington State University. Google Scholar
Fryxell, R., 1962. A radiocarbon limiting date for scabland flooding. Northwest Science. 36, 113-119.Google Scholar
Fryxell, R., 1965. Mazama and Glacier Peak volcanic ash layers—relative ages. Science. 147, 1288-1290.CrossRefGoogle ScholarPubMed
Fryxell, R., 1972. Relationship of late Quaternary volcanic ash layers to geomorphic history of the Columbia Basin, Washington. Geological Society of America Abstracts with Programs. 4, No. 3 159.Google Scholar
Gustafson, C.E., 1976. An ice age lake in the Columbia Basin—new evidence. Geological Society of America Abstracts with Programs. 8, No. 3 377.Google Scholar
Hammatt, H.H., 1976. Late Quaternary stratigraphy and archaeological chronology in the Lower Granite Reservoir, lower Snake River, Washington. Ph. D. dissertation. University of Washington State, 272.Google Scholar
Hammatt, H.H., Foley, L.L., Leonhardy, F.C., 1976. Late Quaternary stratigraphy in the lower Snake River canyon—toward a chronology of slack water sediments. Geological Society of America Abstracts with Programs. 8, No. 3 379.Google Scholar
Moody, U.L., 1976. Late Quaternary stratigraphy of the Lind Coulee and surrounding area. Northwest Science Program and Abstracts, 49th Annual Meeting. Cheney, Wash., March 25–27, 1976 18.Google Scholar
Moody, U.L., 1977. Correlation of flood deposits containing St. Helens set S ashes and the stratigraphic position of St. Helens set J and Glacier Peak ashes, central Washington. Geological Society of America Abstracts with Programs. 9, No. 7 1098-1099.Google Scholar
Mullineaux, D.R., Hyde, J.H., Rubin, M., 1972. Preliminary assessment of upper Pleistocene and Holocene pumiceous tephra from Mount St. Helens, southern Washington. Geological Society of America Abstracts with Programs. 4, No. 3 204-205.Google Scholar
Mullineaux, D.R., Hyde, J.H., Rubin, M., 1975. Widespread late glacial and postglacial tephra deposits from Mount St. Helens volcano. Washington. U. S. Geological Survey Survey Journal of Research. 3, 329-335.Google Scholar
Mullineaux, D.R., Wilcox, R.E., Ebaugh, W.F., Fryxell, R., Rubin, M., 1977. Age of the last major scabland flood of eastern Washington, as inferred from associated ash beds of Mount St. Helens set S. Geological Society of America Abstracts with Programs. 9, No. 7 1105.Google Scholar
Powers, H.A., Wilcox, R.E., 1964. Volcanic ash from Mount Mazama (Crater Lake) and from Glacier Peak. Science. 144, 1334-1336.Google Scholar
Richmond, G.M., Fryxell, R., Neff, G.E., Weis, P.L., 1965. The Cordilleran ice sheet of the northern Rocky Mountains, and related Quaternary history of the Columbia Plateau. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States. Princeton University Press, Princeton, N. J, 231-242.Google Scholar
Rigg, G.B., 1958. Peat resources of Washington. Washington Division of Mines and Geology Bulletin. 44, 272.Google Scholar
Rigg, G.B., Gould, H.R., 1957. Age of Glacier Peak eruption and chronology of post-glacial peat deposits in Washington and surrounding areas. American Journal of Science. 255, 341-363.Google Scholar
Smith, D.G.W., Westgate, J.A., 1969. Electron probe technique for characterizing pyroclastic deposits. Earth and Planetary Science Letters. 5, 313-319.Google Scholar
Smith, H.W., Okazaki, R., Knowles, C.R., 1977. Electron microprobe data for tephra attributed to Glacier Peak, Washington. Quarternary Research. 7, 197-206.Google Scholar
Trimble, D.E., 1963. Geology of Portland, Oregon, and adjacent areas. U. S. Geological Survey Bulletin 1119. 119.Google Scholar
Waitt, R.B. Jr., 1972. Geomorphology and glacial geology of the Methow drainage basin, eastern North Cascade Range, Washington. Ph.D. dissertation. University of Washington, 154.Google Scholar
Waitt, R.B. Jr., 1977. Missoula Flood sans Okanogan Lobe. Geological Society of America Abstracts with Programs. 9, No. 6 770.Google Scholar
Waters, A.C., 1933. Terraces and coulees along the Columbia River near Lake Chelan, Washington. Geological Society of America Bulletin. 44, 783-820.Google Scholar
Westgate, J.A., Fulton, R.J., 1975. Tephrostratigraphy of Olympia interglacial sediments in south-central British Columbia, Canada. Canadian Journal of Earth Sciences. 12, 489-502.Google Scholar
Wilcox, R.E., 1965. Volcanic-ash chronology. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States. Princeton University Press, Princeton, N. J, 807-816.Google Scholar