Coalescing alluvial supporterscone-formed deposits of alluvium that operate jointlyare shaped exactly where rivers arise with the mountains. Once the rivers are large more than enough to extend their courses to The ocean, minimal deltaic plains develop before the supporters; 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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One consequence is that mountain blocks are often bounded by fault scarps and flexure slopes that descend in step development into the adjacent lowlands.