Migration direction of sand-wave structures in pyroclastic-surge deposits: implications for depositional processes

P. D. Cole

doi:10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2

Migration direction of sand-wave structures in pyroclastic-surge deposits: implications for depositional processes

P. D. Cole

Luton College

Research output: Contribution to journal › Article › peer-review

Abstract

Sand-wave structures of both progressive (downstream migrating) and regressive (upstream migrating) types occur within the same pyroclastic-surge deposit at both Roccamonfina volcano (southern Italy) and Sugarloaf Mountain (Arizona, United States). Migration direction of sand waves in these pyroclastic-surge deposits is controlled by the flow regime of the surge cloud rather than the temperature and/or moisture content. -from Author

Original language	English
Pages (from-to)	1108-1111
Journal	Geology
Volume	19
Issue number	11
DOIs	https://doi.org/10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2
Publication status	Published - 1 Jan 1991
Externally published	Yes

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10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2

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title = "Migration direction of sand-wave structures in pyroclastic-surge deposits: implications for depositional processes",

abstract = "Sand-wave structures of both progressive (downstream migrating) and regressive (upstream migrating) types occur within the same pyroclastic-surge deposit at both Roccamonfina volcano (southern Italy) and Sugarloaf Mountain (Arizona, United States). Migration direction of sand waves in these pyroclastic-surge deposits is controlled by the flow regime of the surge cloud rather than the temperature and/or moisture content. -from Author",

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doi = "10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2",

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AU - Cole, P. D.

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N2 - Sand-wave structures of both progressive (downstream migrating) and regressive (upstream migrating) types occur within the same pyroclastic-surge deposit at both Roccamonfina volcano (southern Italy) and Sugarloaf Mountain (Arizona, United States). Migration direction of sand waves in these pyroclastic-surge deposits is controlled by the flow regime of the surge cloud rather than the temperature and/or moisture content. -from Author

AB - Sand-wave structures of both progressive (downstream migrating) and regressive (upstream migrating) types occur within the same pyroclastic-surge deposit at both Roccamonfina volcano (southern Italy) and Sugarloaf Mountain (Arizona, United States). Migration direction of sand waves in these pyroclastic-surge deposits is controlled by the flow regime of the surge cloud rather than the temperature and/or moisture content. -from Author

U2 - 10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2

DO - 10.1130/0091-7613(1991)019<1108:MDOSWS>2.3.CO;2

M3 - Article

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VL - 19

SP - 1108

EP - 1111

JO - Geology

JF - Geology

IS - 11

ER -

Migration direction of sand-wave structures in pyroclastic-surge deposits: implications for depositional processes

Abstract

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