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  2. 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 ]

  3. William Morris Davis - Wikipedia

    en.wikipedia.org/wiki/William_Morris_Davis

    Though the cycle of erosion was a crucial early contribution to the development of geomorphology, many of Davis' theories regarding landscape evolution, sometimes termed 'Davisian geomorphology', were heavily criticized by later geomorphologists. When Davis retired from Harvard in 1911, the study of landscape evolution was nearly monopolized by ...

  4. Lester Charles King - Wikipedia

    en.wikipedia.org/wiki/Lester_Charles_King

    While King's ideas were an attempt at refuting Davis' cycle of erosion they were themselves of cyclical nature and contributed to what Cliff Ollier has called "Davis bashing" — the ridicule of cyclical theories in geomorphology, in particular Davis' ones. Critics did however not propose alternative models. [1]

  5. Denudation chronology - Wikipedia

    en.wikipedia.org/wiki/Denudation_chronology

    Denudation chronology revolves around episodes of landscape-wide erosion, better known as denudation. The cycle of erosion model is a common approach used to establish denudation chronologies. [ 1 ]

  6. Geomorphology - Wikipedia

    en.wikipedia.org/wiki/Geomorphology

    The inherent difficulties of the model have instead made geomorphological research to advance along other lines. [46] In contrast to its disputed status in geomorphology, the cycle of erosion model is a common approach used to establish denudation chronologies, and is thus an important concept in the science of historical geology. [48]

  7. Hillslope evolution - Wikipedia

    en.wikipedia.org/wiki/Hillslope_evolution

    This model show that when ∇z is far from S c it behaves like equation 1. On the contrary when ∇z approaches S c erosion rates becomes extremely high. This last feature may represent the behavior of landslides in steep terrain. [7] At low erosion rates increased stream or river incision may make gentle slopes

  8. Universal Soil Loss Equation - Wikipedia

    en.wikipedia.org/wiki/Universal_Soil_Loss_Equation

    The Universal Soil Loss Equation (USLE) is a widely used mathematical model that describes soil erosion processes. [1]Erosion models play critical roles in soil and water resource conservation and nonpoint source pollution assessments, including: sediment load assessment and inventory, conservation planning and design for sediment control, and for the advancement of scientific understanding.

  9. Erosion prediction - Wikipedia

    en.wikipedia.org/wiki/Erosion_prediction

    A few erosion models focus on erosion on mined areas. The aim of the majority of soil erosion models is to predict average rates (often an annual average rate) of soil loss from an area such as a plot, a field or a catchment/watershed under various land management techniques. Some erosion models are purely statistical, others more mechanistic ...

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