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  2. Isostasy - Wikipedia

    en.wikipedia.org/wiki/Isostasy

    Airy and Pratt isostasy are statements of buoyancy, but flexural isostasy is a statement of buoyancy when deflecting a sheet of finite elastic strength. In other words, the Airy and Pratt models are purely hydrostatic, taking no account of material strength, while flexural isostacy takes into account elastic forces from the deformation of the ...

  3. Mass wasting - Wikipedia

    en.wikipedia.org/wiki/Mass_wasting

    Mass wasting, also known as mass movement, [1] is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in a moving medium, such as water, wind, or ice.

  4. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    This is in recognition that the response of the Earth to glacial loading and unloading is not limited to the upward rebound movement, but also involves downward land movement, horizontal crustal motion, [3] [6] changes in global sea levels [7] and the Earth's gravity field, [8] induced earthquakes, [9] and changes in the Earth's rotation. [10]

  5. Tectonic uplift - Wikipedia

    en.wikipedia.org/wiki/Tectonic_uplift

    The removal of mass from a region will be isostatically compensated by crustal rebound. If we take into consideration typical crustal and mantle densities, erosion of an average 100 meters of rock across a broad, uniform surface will cause the crust to isostatically rebound about 85 meters and will cause only a 15-meter loss of mean surface ...

  6. Glacier mass balance - Wikipedia

    en.wikipedia.org/wiki/Glacier_mass_balance

    Ablation is the reverse of accumulation: it includes all the processes by which a glacier can lose mass. The main ablation process for most glaciers that are entirely land-based is melting; the heat that causes melting can come from sunlight, or ambient air, or from rain falling on the glacier, or from geothermal heat below the glacier bed.

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  8. Solifluction - Wikipedia

    en.wikipedia.org/wiki/Solifluction

    Solifluction is a collective name for gradual processes in which a mass moves down a slope ("mass wasting") related to freeze-thaw activity. This is the standard modern meaning of solifluction, which differs from the original meaning given to it by Johan Gunnar Andersson in 1906. [1] [2]

  9. Trump picks Navarro to be senior counselor for trade and ...

    www.aol.com/news/trump-picks-navarro-senior...

    WASHINGTON (Reuters) -U.S. President-elect Donald Trump said on Wednesday he had picked Peter Navarro to be senior counselor for trade and manufacturing. Navarro served as head of a newly created ...

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