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  2. Flared slope - Wikipedia

    en.wikipedia.org/wiki/Flared_slope

    Part of a larger inselberg, Hyden Rock, Wave Rock holds many distinct characteristics that make it a target for understanding flared slope formations. [3] Because Wave Rock contains various distinct shapes and curves within its structure, it is thought to have formed from multiple processes, including due to marine erosion, sand blasting, and ...

  3. Coastal erosion - Wikipedia

    en.wikipedia.org/wiki/Coastal_erosion

    [1] [2] The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. [3] Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. [3]

  4. Stack (geology) - Wikipedia

    en.wikipedia.org/wiki/Stack_(geology)

    A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. [1] Stacks are formed over time by wind and water, processes of coastal geomorphology. [2]

  5. Wave pounding - Wikipedia

    en.wikipedia.org/wiki/Wave_pounding

    Wave pounding is a force of erosion along coast lines. The effects of wave pounding are influenced by wave shape, ocean chemistry , rock type, and morphology of the coastal landscape. There are three different types of waves to consider in this process: spilling, plunging, and surging waves.

  6. Dynamic revetment - Wikipedia

    en.wikipedia.org/wiki/Dynamic_revetment

    Bayocean, Oregon, January 2020. Dynamic revetments, also known as "cobble berms" or "dynamic cobble berm revetments", use gravel or cobble-sized rocks to mimic a natural cobble storm beach for the purpose of reducing wave energy and stopping or slowing coastal erosion. [1]

  7. Erosion - Wikipedia

    en.wikipedia.org/wiki/Erosion

    Erosion and changes in the form of river banks may be measured by inserting metal rods into the bank and marking the position of the bank surface along the rods at different times. [23] Thermal erosion is the result of melting and weakening permafrost due to moving water. [24] It can occur both along rivers and at the coast.

  8. Beach evolution - Wikipedia

    en.wikipedia.org/wiki/Beach_evolution

    The port of Ephesus, one of the great cities of the Ionian Greeks in Asia Minor, was filled with sediment due to accretion from a nearby river; it is now 5 kilometers (3.1 mi) from the sea. Likewise, Ostia , the once-important port near ancient Rome , is now several kilometres inland, the coastline having moved slowly seaward.

  9. Submersion (coastal management) - Wikipedia

    en.wikipedia.org/wiki/Submersion_(coastal...

    The term erosion often is associated with undesirable impacts on the environment, whereas submersion is a sustainable part of healthy foreshores. Communities making decisions about coastal management need to develop understanding of the components of beach recession and be able to separate the component that is temporary sustainable submersion from the more serious irreversible anthropogenic ...