Coalescing alluvial fanscone-formed deposits of alluvium that run collectivelyare formed where rivers arise through the mountains. Once the rivers are significant more than enough to extend their courses to The ocean, minimal deltaic plains develop before the followers; this happens most frequently where the rivers vacant into shallow and sheltered bays, as within the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.

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Just one 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.