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  2. Denudation - Wikipedia

    en.wikipedia.org/wiki/Denudation

    Denudation has a large impact on karst and landscape evolution because the most-rapid changes to landscapes occur when there are changes to subterranean structures. [36] Other research includes effects on denudation rates; this research is mostly studying how climate [37] and vegetation [38] impact denudation.

  3. Soil erosion - Wikipedia

    en.wikipedia.org/wiki/Soil_erosion

    Soil erosion is the denudation or wearing away of the upper layer of soil. It is a form of soil degradation. This natural process is caused by the dynamic activity of erosive agents, that is, water, ice (glaciers), snow, air (wind), plants, and animals (including humans).

  4. Exhumation (geology) - Wikipedia

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

    Exhumation through denudation could be considered as the process of exposing rock packages solely through the removal of their overlying unconsolidated sediments or solid rock layers. Denudation is here considered as a process that removes parts of the Earth's upper crust by physical processes that occur naturally (e.g. glaciers , wind, water ...

  5. Denudation chronology - Wikipedia

    en.wikipedia.org/wiki/Denudation_chronology

    Denudation chronology is the study of the long-term evolution of topography seen as sequence. 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.

  6. 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]

  7. River terraces (tectonic–climatic interaction) - Wikipedia

    en.wikipedia.org/wiki/River_terraces_(tectonic...

    A schematic diagram of the morphology of coastal/marine terraces. Periodic uplift will force old shorelines up, which create the terrace treads. Wave erosion on these old shorelines will produce the scarp, or terrace riser. A satellite image of the Himalayas and the rainshadow effect.

  8. Peneplain - Wikipedia

    en.wikipedia.org/wiki/Peneplain

    The existence of some peneplains, and peneplanation as a process in nature, is not without controversy, due to a lack of contemporary examples and uncertainty in identifying relic examples. [ 1 ] [ 4 ] By some definitions, peneplains grade down to a base level represented by sea level , yet in other definitions such a condition is ignored. [ 4 ]

  9. File:Diagram of the water cycle including some human activity.pdf

    en.wikipedia.org/wiki/File:Diagram_of_the_water...

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