Paleoflood hydrologic analysis from slack-water deposits.

V. R. Baker

Paleoflood hydrologic analysis from slack-water deposits.

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Abstract

Slack-water sedimentation analysis has been successfully applied to the paleohydrologic interpretation of the late Pleistocene Missoula floods (13 000 ¹⁴C yr BP in the northwestern US). It is especially useful in Holocene studies, as demonstrated by work in semi-arid regions (Texas, Utah, northern Australia) and humid temperate regions (Connecticut, Virginia, Pennsylvania). -from Author

Original language	English (US)
Pages (from-to)	19-26
Number of pages	8
Journal	Quaternary Studies in Poland
Volume	4
State	Published - 1983

ASJC Scopus subject areas

Geology

Cite this

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abstract = "Slack-water sedimentation analysis has been successfully applied to the paleohydrologic interpretation of the late Pleistocene Missoula floods (13 000 14C yr BP in the northwestern US). It is especially useful in Holocene studies, as demonstrated by work in semi-arid regions (Texas, Utah, northern Australia) and humid temperate regions (Connecticut, Virginia, Pennsylvania). -from Author",

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AB - Slack-water sedimentation analysis has been successfully applied to the paleohydrologic interpretation of the late Pleistocene Missoula floods (13 000 14C yr BP in the northwestern US). It is especially useful in Holocene studies, as demonstrated by work in semi-arid regions (Texas, Utah, northern Australia) and humid temperate regions (Connecticut, Virginia, Pennsylvania). -from Author

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Paleoflood hydrologic analysis from slack-water deposits.

Abstract

ASJC Scopus subject areas

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