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  2. Denudation - Wikipedia

    en.wikipedia.org/wiki/Denudation

    Although the terms erosion and denudation are used interchangeably, erosion is the transport of soil and rocks from one location to another, [1] and denudation is the sum of processes, including erosion, that result in the lowering of Earth's surface. [2]

  3. Soil erosion - Wikipedia

    en.wikipedia.org/wiki/Soil_erosion

    Soil erosion may be a slow process that continues relatively unnoticed, or it may occur at an alarming rate causing a serious loss of topsoil. The loss of soil from farmland may be reflected in reduced crop production potential, lower surface water quality and damaged drainage networks. Soil erosion could also cause sinkholes.

  4. Erosion - Wikipedia

    en.wikipedia.org/wiki/Erosion

    Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement.

  5. Exhumation (geology) - Wikipedia

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

    Exhumation of buried rocks should be considered as two different categories namely, exhumation by denudation/erosion or exhumation by tectonic processes followed by erosion. In the latter case, rocks (or rock packages) from deeper crustal levels (meter to kilometer depths below the Earth's surface) are brought towards the Earth's surface (i.e ...

  6. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    The materials left after the rock breaks down combine with organic material to create soil. Many of Earth's landforms and landscapes are the result of weathering, erosion and redeposition. Weathering is a crucial part of the rock cycle ; sedimentary rock , the product of weathered rock, covers 66% of the Earth's continents and much of the ocean ...

  7. Cycle of erosion - Wikipedia

    en.wikipedia.org/wiki/Cycle_of_erosion

    The geographic cycle, or cycle of erosion, is an idealized model that explains the development of relief in landscapes. [1] The model starts with the erosion that follows uplift of land above a base level and ends, if conditions allow, in the formation of a peneplain . [ 1 ]

  8. California's piers may not be able to withstand climate change

    www.aol.com/news/californias-piers-may-not-able...

    Climate change continues to worsen the coastal storms that batter California's aging piers. The result is frequent and expensive repairs.

  9. Erodibility - Wikipedia

    en.wikipedia.org/wiki/Erodibility

    Erodability (or erodibility) is the inherent yielding or nonresistance of soils and rocks to erosion. A high erodibility implies that the same amount of work exerted by the erosion processes leads to a larger removal of material. Because the mechanics behind erosion depend upon the competence and coherence of the material, erodibility is ...