Coalescing alluvial supporterscone-shaped deposits of alluvium that operate alongside one anotherare fashioned the place rivers emerge within the mountains. If the rivers are huge sufficient to increase their programs to The ocean, lower deltaic plains build before the enthusiasts; this occurs most often exactly where the rivers vacant into shallow and sheltered bays, as while in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.

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One particular consequence is the fact mountain blocks in many cases are bounded by fault scarps and flexure slopes that descend in action development on the adjacent lowlands.