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River systems of young erosional cycle typical of dissected mountain terrain with intense manifestation of the latest tectonic movements, giving rise to the active development of river valleys. Longitudinal profile of the equilibrium of such river systems is not exhausted, so the processes of erosion and denudation dominate over their accumulation, and river valleys are experiencing phases of deepening, partly - the expansion, is formed by sharply dissected terrain with deeply incised river valleys, steep sides. Under these conditions dominate the processes of bottom and lateral erosion, which resulted in the collapse of indigenous mineralized zones in the sides and their heads are destroyed terraces placer previous erosion cycles. In such circumstances, the resulting dominant transportation of clastic material, and the river bed facies are coarse and pebbly gravel and sand deposits. Notes the active flow of useful components in modern alluvium - there is an active modern ore drift. |