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Relief formation and erosion during the Quaternary period

Relief formation and erosion during the Quaternary period

Pochvovedenie (6): 67-78

A general theory of erosion-aggradation processes is proposed, which explains the genesis of loessial rocks on water divides and slopes, and the formation of slopes and mantle deposits. It links the distribution of forest and grass (steppe) vegetation and its corresponding soils with the hydrogeological characteristics of loess beds.

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Accession: 000734836

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