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In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material, and rises from the bed of a body of water close to the surface or above it, which poses a danger to navigation.
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.
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 ...
Shoal, also known as bar – Natural submerged sandbank that rises from a body of water to near the surface; Spring (hydrology) – Point at which water emerges from an aquifer to the surface; Stream – Body of surface water flowing down a channel; Stream pool – Deep and slow-moving stretch of a watercourse
Paleoplain - A buried erosion plain; a particularly large and flat erosion surface; Panhole – Depression or basin eroded into flat or gently sloping cohesive rock; Pediment – Very gently sloping inclined bedrock surface; Pediplain – Extensive plain formed by the coalescence of pediments; Peneplain – Low-relief plain formed by protracted ...
Accretion is the process of coastal sediment returning to the visible portion of a beach or foreshore after a submersion event. [1] A sustainable beach or foreshore often goes through a cycle of submersion during rough weather and later accretion during calmer periods.
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.
A graded shoreline is a stage in the cycle of coastal development characterised by a flat and straight coastline.It is formed under the influence of wind and water from the original bays, islands, peninsulas and promontories.