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  2. Sheet erosion - Wikipedia

    en.wikipedia.org/wiki/Sheet_Erosion

    Sheet erosion or sheet wash is the even erosion of substrate along a wide area. [1] It occurs in a wide range of settings such as coastal plains , hill slopes, floodplains , beaches , [ 2 ] savanna plains [ 3 ] and semi-arid plains. [ 4 ]

  3. Surface runoff - Wikipedia

    en.wikipedia.org/wiki/Surface_runoff

    Surface runoff can cause erosion of the Earth's surface; eroded material may be deposited a considerable distance away. There are four main types of soil erosion by water: splash erosion, sheet erosion, rill erosion and gully erosion. Splash erosion is the result of mechanical collision of raindrops with the soil surface: soil particles which ...

  4. Soil erosion - Wikipedia

    en.wikipedia.org/wiki/Soil_erosion

    Splash erosion is generally seen as the first and least severe stage in the soil erosion process, which is followed by sheet erosion, then rill erosion and finally gully erosion (the most severe of the four). [6] [7] In splash erosion, the impact of a falling raindrop creates a small crater in the soil, [8] ejecting soil particles. [9]

  5. Erosion - Wikipedia

    en.wikipedia.org/wiki/Erosion

    Erosion of mountains massifs can create a pattern of equally high summits called summit accordance. [73] It has been argued that extension during post-orogenic collapse is a more effective mechanism of lowering the height of orogenic mountains than erosion. [74] Examples of heavily eroded mountain ranges include the Timanides of

  6. Rill - Wikipedia

    en.wikipedia.org/wiki/Rill

    Landscape shaped by rill erosion. Volgograd Oblast, Russia. Although rills are small, they transport significant amounts of soil each year. Some estimates claim rill flow has a carrying capacity of nearly ten times that of non-rill, or interrill, areas. In a moderate rainfall, rill flow can carry rock fragments up to 9 cm in diameter downslope.

  7. Pediment (geology) - Wikipedia

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

    Sheetwash or sheet erosion, in which broad sheets of flowing water evenly remove thin layers of surface material without incising channels. [18] [19] Mountain-front retreating by weathering [20] Lateral planation or erosion by a stream [21] Rillwash or rill erosion, in which flow is concentrated in numerous closely spaced minute channels. [19]

  8. Erosion control - Wikipedia

    en.wikipedia.org/wiki/Erosion_control

    Erosion control is the practice of preventing or controlling wind or water erosion in agriculture, land development, coastal areas, river banks and construction. Effective erosion controls handle surface runoff and are important techniques in preventing water pollution , soil loss , wildlife habitat loss and human property loss.

  9. Fluvial sediment processes - Wikipedia

    en.wikipedia.org/wiki/Fluvial_sediment_processes

    The erosion associated with overland flow may occur through different methods depending on meteorological and flow conditions. If the initial impact of rain droplets dislodges soil, the phenomenon is called rainsplash erosion. If overland flow is directly responsible for sediment entrainment but does not form gullies, it is called "sheet erosion".

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