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  2. Shingle beach - Wikipedia

    en.wikipedia.org/wiki/Shingle_beach

    A shingle beach in Batanes, Philippines Pebbles on a shingle beach in Somerset, England Shingle Beach in Hillsburn, Nova Scotia, Canada. A shingle beach, also known as either a cobble beach or gravel beach, is a commonly narrow beach that is composed of coarse, loose, well-rounded, and waterworn gravel, called shingle.

  3. Template:Coastal geography - Wikipedia

    en.wikipedia.org/wiki/Template:Coastal_geography

    A navigational box that can be placed at the bottom of articles. Template parameters [Edit template data] Parameter Description Type Status State state The initial visibility of the navbox Suggested values collapsed expanded autocollapse String suggested Template transclusions Transclusion maintenance Check completeness of transclusions The above documentation is transcluded from Template ...

  4. Coastal geography - Wikipedia

    en.wikipedia.org/wiki/Coastal_geography

    Collapsed Ordovician limestone bank showing coastal erosion.NW Osmussaar, Estonia.. Coastal geography is the study of the constantly changing region between the ocean and the land, incorporating both the physical geography (i.e. coastal geomorphology, climatology and oceanography) and the human geography (sociology and history) of the coast.

  5. Storm beach - Wikipedia

    en.wikipedia.org/wiki/Storm_beach

    The resultant landform is often a very steep beach (up to 45°) composed of rounded cobbles, shingle and occasionally sand. The stones usually have an obvious grading of pebbles, from large to small, with the larger diameter stones typically arrayed at the highest beach elevations. It may also contain many small parts of shipwrecked boats.

  6. Coastal morphodynamics - Wikipedia

    en.wikipedia.org/wiki/Coastal_morphodynamics

    As sediment takes a finite time to move, there is a lag in the morphological response to hydrodynamic forcing. Sediment can therefore be considered to be a time-dependent coupling mechanism. Since the boundary conditions of hydrodynamic forcing change regularly, this may mean that the beach never attains equilibrium. Morphodynamic processes ...

  7. Beach cusps - Wikipedia

    en.wikipedia.org/wiki/Beach_cusps

    In the adjacent diagram, the two waves cancel each other out, creating a flat surface. However, this is a highly simplified version of events. The incoming wave has the same wave period as the edge wave, so the incoming wave changes from a peak to a trough over the same period as it takes the standing wave to change so they keep the same pattern.

  8. The Shingle House (Style Spotlight) - AOL

    www.aol.com/news/2012-07-11-the-shingled-house...

    Like a balloon, the Shingle style exterior was all taut and tensioned to hold the interior space in place. The Shingle style fell out of favor at the turn of the 20th century when the Colonial ...

  9. File:Accreting coast Image6.svg - Wikipedia

    en.wikipedia.org/wiki/File:Accreting_coast_Image...

    This work has been released into the public domain by its author, Feydey.This applies worldwide. In some countries this may not be legally possible; if so: Feydey grants anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law.