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  2. 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 ]

  3. Iribarren number - Wikipedia

    en.wikipedia.org/wiki/Iribarren_number

    The parameter used to describe breaking wave types on beaches; or wave run-up on – and reflection by – beaches, breakwaters and dikes. [4] [5] [6] Iribarren Number (ξ 0) as a function of wave height with constant beach steepness of 7.5 degrees. Iribarren's work was further developed by Jurjen Battjes in 1974, who named the parameter after ...

  4. Coastal erosion - Wikipedia

    en.wikipedia.org/wiki/Coastal_erosion

    Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. [3] On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion.

  5. 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.

  6. Beach evolution - Wikipedia

    en.wikipedia.org/wiki/Beach_evolution

    Beach evolution is a natural process occurring along shorelines where sea, lake or river water erodes the land. Beaches form as sand accumulates over centuries through recurrent processes that erode rocky and sedimentary material into sand deposits.

  7. Surtsey - Wikipedia

    en.wikipedia.org/wiki/Surtsey

    However, eruptions more than kept pace with wave erosion, and by February 1964, the island had a maximum diameter of over 1,300 metres (4,265 feet). [ 5 ] The explosive phreatomagmatic eruptions caused by the easy access of water to the erupting vents threw rocks up to a kilometre (0.6 mi) away from the island, and sent ash clouds as high as 10 ...

  8. Dynamic revetment - Wikipedia

    en.wikipedia.org/wiki/Dynamic_revetment

    Unlike seawalls, dynamic revetment is designed to allow wave action to rearrange the stones into an equilibrium profile, disrupting wave action and dissipating wave energy as the cobbles move. This can reduce the wave reflection which often contributes to beach scouring .

  9. Category:Erosion - Wikipedia

    en.wikipedia.org/wiki/Category:Erosion

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