Coalescing alluvial enthusiastscone-shaped deposits of alluvium that operate togetherare fashioned the place rivers emerge from the mountains. If the rivers are huge sufficient to increase their programs to the sea, very low deltaic plains build before the enthusiasts; this occurs most often in which the rivers vacant into shallow and sheltered bays, as while in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.

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A person consequence is that mountain blocks are often bounded by fault scarps and flexure slopes that descend in step development into the adjacent lowlands.