Coalescing alluvial admirerscone-shaped deposits of alluvium that operate collectivelyare fashioned exactly where rivers arise within the mountains. Once the rivers are substantial sufficient to extend their classes to the sea, minimal deltaic plains acquire before the followers; this happens most often where the rivers empty into shallow and sheltered bays, as from the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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One particular consequence is mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in step development for the adjacent lowlands.