Coalescing alluvial fanscone-formed deposits of alluvium that operate jointlyare shaped exactly where rivers arise through the mountains. Once the rivers are significant plenty of to extend their courses to The ocean, reduced deltaic plains establish before the followers; this happens most frequently where by the rivers empty into shallow and sheltered bays, as within the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.

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One consequence is that mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in step formation into the adjacent lowlands.