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  2. Blowout (geomorphology) - Wikipedia

    en.wikipedia.org/wiki/Blowout_(geomorphology)

    Disturbances are general phrases which define a cause that creates an exposure in the vegetative skin to eventually form a blowout formation. Rather than being described as events, disturbances are terms which describe the rate at which breaches create an opening and expand, yet there are numerous types of disturbances that can penetrate the protective vegetative skin.

  3. Aeolian landform - Wikipedia

    en.wikipedia.org/wiki/Aeolian_landform

    A dune is a large pile of wind-blown material, typically sand or snow. As the pile accumulates, its larger surface area increases the rate of deposition in a positive feedback loop until the dune collapses under its own weight. This process causes dunes to move in the direction of the wind over time. [6] [7] Death Valley Mesquite Flats sand dunes.

  4. Interdunal wetland - Wikipedia

    en.wikipedia.org/wiki/Interdunal_wetland

    An interdunal wetland, interdunal pond or dune slack is a water-filled depression between coastal sand dunes. It may be formed either by wind erosion or by dunal encroachment on an existing wetland. [1] The wind erosion process involves wind scooping out sufficient sand to reach the water table, and typically occurs behind the first line of ...

  5. The Physics of Blown Sand and Desert Dunes - Wikipedia

    en.wikipedia.org/wiki/The_Physics_of_Blown_Sand...

    The Physics of Blown Sand and Desert Dunes is a scientific book written by Ralph A. Bagnold. [1] The book laid the foundations of the scientific investigation of the transport of sand by wind. [2] It also discusses the formation and movement of sand dunes in the Libyan Desert.

  6. Erg (landform) - Wikipedia

    en.wikipedia.org/wiki/Erg_(landform)

    Erg Chebbi, Morocco Major dune seas of the Sahara in yellow, Great Sand Sea.Red dashed line shows approximate limit of the Sahara. Sand seas and dune fields generally occur in regions downwind of copious sources of dry, loose sand, such as dry riverbeds and deltas, floodplains, glacial outwash plains, dry lakes, and beaches.

  7. Barchan - Wikipedia

    en.wikipedia.org/wiki/Barchan

    As barchan dunes migrate, smaller dunes outpace larger dunes, catching-up the rear of the larger dune and eventually appear to punch through the large dune to appear on the other side. The process appears superficially similar to waves of light, sound, or water that pass directly through each other, but the detailed mechanism is very different.

  8. How to Read All the 'Dune' Books in Order - AOL

    www.aol.com/read-dune-books-order-160800257.html

    In Dune, Oregon turns to Arrakis, the desert prophets of the past make way for a young Paul Atreides, and the science of ecology is still very much the science of ecology—the highest function of ...

  9. Dune - Wikipedia

    en.wikipedia.org/wiki/Dune

    A large dune complex is called a dune field, [7] while broad, flat regions covered with wind-swept sand or dunes, with little or no vegetation, are called ergs or sand seas. [ 8 ] [ 9 ] [ 10 ] Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have ...

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