Search Results - "Krapf, Carmen B.E."

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  1. 1

    Sedimentology and architecture of the Douglas Creek terminal splay, Lake Eyre, central Australia by FISHER, JOHN A, KRAPF, CARMEN B.E, LANG, SIMON C, NICHOLS, GARY J, PAYENBERG, TOBIAS H.D

    Published in Sedimentology (01-12-2008)
    “…Douglas Creek terminal splay, sited on the western shoreline of Lake Eyre North, central Australia, covers a surface area of approximately 4 km² with a…”
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  2. 2

    Mass and hyperconcentrated flow deposits record dune damming and catastrophic breakthrough of ephemeral rivers, Skeleton Coast Erg, Namibia by Svendsen, Johan, Stollhofen, Harald, Krapf, Carmen B.E, Stanistreet, Ian G

    Published in Sedimentary geology (01-08-2003)
    “…Channel-shaped deposits of well sorted sand with only 2–4% fine-grained material, being either massive and structureless or upward fining with basal lag, are…”
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  3. 3

    The interplay of fluvial, lacustrine and aeolian deposition and erosion along the Neales Cliffs and its relevance to the evolution of Kati Thanda-Lake Eyre, central Australia, during the Quaternary by Krapf, Carmen B.E., Lang, Simon C., Werner, Mario

    “…A high-resolution record of fluvial, aeolian and lacustrine deposits of Late Pleistocene age is exposed along the Neales Cliff in the lower reaches of the…”
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  4. 4

    Contrasting styles of ephemeral river systems and their interaction with dunes of the Skeleton Coast erg (Namibia) by Krapf, Carmen B.E., Stollhofen, Harald, Stanistreet, Ian G.

    Published in Quaternary international (2003)
    “…The Skeleton Coast erg forms a prominent NNW trending dune belt, 6– 22 km wide, comprising dunes up to 50 m high, sub-parallel to the South Atlantic margin of…”
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  5. 5

    A quantitative model for deposition of thin fluvial sand sheets by Fisher, John A, Waltham, David, Nichols, Gary J, Krapf, Carmen B. E, Lang, Simon C

    Published in Journal of the Geological Society (01-01-2007)
    “…Sheetfloods are typically invoked as the mechanism responsible for the kilometre-scale transport of sand-sized sediment grains in shallow-gradient fluvial…”
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