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  2. Blowout (geomorphology) - Wikipedia

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

    Blowout located 6.5 km south of Earth, Texas (1996). Blowouts are sandy depressions in a sand dune ecosystem caused by the removal of sediments by wind.. Commonly found in coastal settings and margins of arid areas, blowouts tend to form when wind erodes patches of bare sand on stabilized vegetated dunes.

  3. Aeolian landform - Wikipedia

    en.wikipedia.org/wiki/Aeolian_landform

    Dunes: 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 ...

  4. 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 ...

  5. Erg (landform) - Wikipedia

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

    The sand dunes are believed to be formed by wind generated as a result of tidal forces from Saturn on Titan's atmosphere. The images are evidence that these dunes were built from winds that blow in one direction before switching to another and then back to the first direction and so on, causing the sand dunes to build up in long parallel lines.

  6. Cross-bedding - Wikipedia

    en.wikipedia.org/wiki/Cross-bedding

    Cross-bedding is formed by the downstream migration of bedforms such as ripples or dunes [3] in a flowing fluid. The fluid flow causes sand grains to saltate up the stoss (upstream) side of the bedform and collect at the peak until the angle of repose is reached. At this point, the crest of granular material has grown too large and will be ...

  7. Scientists reveal secrets of Earth's magnificent desert star ...

    www.aol.com/news/scientists-reveal-secrets-earth...

    They are among the wonders of our deserts: star dunes, the vaguely pyramid-shaped sand formations up to about 1,000 feet (300 meters) tall with arms stretching out from a central peak to give them ...

  8. Barchan - Wikipedia

    en.wikipedia.org/wiki/Barchan

    Simple barchan dunes may appear as larger, compound barchan or megabarchan dunes, which can gradually migrate with the wind as a result of erosion on the windward side and deposition on the leeward side, at a rate of migration ranging from about one meter to 100 meters per year. Barchans usually occur as groups of isolated dunes and may form ...

  9. Star dune: Scientists solve mystery behind Earth's largest ...

    www.aol.com/star-dune-scientists-solve-mystery...

    Scientists collected radioactive sand grains in the dark to understand when they formed. Star dune: Scientists solve mystery behind Earth's largest desert sands Skip to main content