Coalescing alluvial followerscone-formed deposits of alluvium that operate jointlyare shaped exactly where rivers arise with the mountains. Once the rivers are large enough to increase 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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A single consequence is mountain blocks are frequently bounded by fault scarps and flexure slopes that descend in phase formation for the adjacent lowlands.