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  2. Denudation - Wikipedia

    en.wikipedia.org/wiki/Denudation

    Download QR code; Print/export Download as PDF; Printable version; In other projects ... Denudation is the geological process in which moving water, ...

  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. 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.

  5. 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]

  6. Exhumation (geology) - Wikipedia

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

    Exhumation by tectonic processes refers to any geological mechanism that brings rocks from deeper crustal levels to shallower crustal levels. While erosion or denudation is fundamental in eventually exposing these deeper rocks at the Earth's surface, the geological phenomenon that drive the rocks to shallower crust are still considered exhumation processes.

  7. Geomorphology - Wikipedia

    en.wikipedia.org/wiki/Geomorphology

    Denudation of these high uplifted regions produces sediment that is transported and deposited elsewhere within the landscape or off the coast. [3] On progressively smaller scales, similar ideas apply, where individual landforms evolve in response to the balance of additive processes (uplift and deposition) and subtractive processes ( subsidence ...

  8. 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.

  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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