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The lack of vegetation exposes the unprotected surface of the ground to the processes of denudation.
Representing the end-products of weathering, denudation, and soil formation, duricrusts occur mainly on erosional platforms such as pediments or as cappings and residuals on stream divides.
Such processes play an essential and conspicuous role in the denudation of land surfaces and the transport of rock detritus from higher to lower levels.
Land degradation was a serious problem in the Tigray Region with severe denudation of vegetation cover, depletion of soil fertility, and deterioration of surface and ground water potential (Berhanu et al. 2003).
Karst ends with denudation at the Earth's surface.
Eventually the denudation of the land surface destroys the last vestiges of the passages, bringing to an end the long history of the cave conduit.
Beginning in 1899, Davis proposed that denudation of the land occurs in what he called "the geographical cycle".
Continents are first-order landforms, and there seemingly will be only one cycle of continental denudation in the history of the Earth.
Accurate determination of denudation rates is important in understanding Earth surface system dynamics.
Major impacts to lowlands include denudation of vegetation cover and organic horizons, an increase in active-layer depth, and ground subsidence or deflation (Lawson 1986); (Slaughter and others 1990); (Racine and Ahlstrand 1991).
Denudation intensified after the Pliocene.
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