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  2. Soil erosion - Wikipedia

    en.wikipedia.org/wiki/Soil_erosion

    Soil erosion could also cause sinkholes. ... down the slope. [10] Sheet erosion is the transport of loosened soil particles by overland flow. ...

  3. Downhill creep - Wikipedia

    en.wikipedia.org/wiki/Downhill_creep

    Downhill creep, also known as soil creep or commonly just creep, is a type of creep characterized by the slow, downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress.

  4. Slope stability - Wikipedia

    en.wikipedia.org/wiki/Slope_stability

    Slope stability refers to the condition of inclined soil or rock slopes to withstand or undergo movement; the opposite condition is called slope instability or slope failure. The stability condition of slopes is a subject of study and research in soil mechanics , geotechnical engineering , and engineering geology .

  5. Erosion - Wikipedia

    en.wikipedia.org/wiki/Erosion

    If the runoff has sufficient flow energy, it will transport loosened soil particles down the slope. [15] Sheet erosion is the transport of loosened soil particles by overland flow. [15] A spoil tip covered in rills and gullies due to erosion processes caused by rainfall: Rummu, Estonia

  6. Tillage erosion - Wikipedia

    en.wikipedia.org/wiki/Tillage_Erosion

    Eroded hilltops due to tillage erosion. Tillage erosion is a form of soil erosion occurring in cultivated fields due to the movement of soil by tillage. [1] [2] There is growing evidence that tillage erosion is a major soil erosion process in agricultural lands, surpassing water and wind erosion in many fields all around the world, especially on sloping and hilly lands [3] [4] [5] A signature ...

  7. Soil sloughing - Wikipedia

    en.wikipedia.org/wiki/Soil_sloughing

    Due to precipitation, seasonal changes in Water content can lead to soil sloughing. [7] Soil sloughing is also an indicator of active soil movement and frequently requires action to reduce or prevent bank and slope failure. Soil water content is highly related to the mass erosion that leads to soil sloughing or even slopes failure. [7]

  8. Erodibility - Wikipedia

    en.wikipedia.org/wiki/Erodibility

    where R is the rainfall erosivity factor, K is the soil erodibility, [3] [4] L and S are topographic factors representing length and slope, and C and P are cropping management factors. Other factors such as the stone content (referred as stoniness), which acts as protection against soil erosion, are very significant in Mediterranean countries.

  9. Gully - Wikipedia

    en.wikipedia.org/wiki/Gully

    Gravity causes rift erosion on a downward slope, with steeper slopes generating greater water flow. Sandier terrains are more commonly affected by rills most prevalent during the rainier months. Gullies develop when a rill is neglected for an extended time, thickening and expanding as soil erosion persists. [5]