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 |
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Pages (from-to) | 1108-1111 |
Number of pages | 0 |
Journal | Geology |
Volume | 19 |
Issue number | 11 |
DOIs | |
Publication status | Published - 1 Jan 1991 |