Coalescing alluvial enthusiastscone-shaped deposits of alluvium that run with each otherare formed where by rivers arise in the mountains. When the rivers are substantial ample to extend their classes to the sea, reduced deltaic plains establish before the followers; this occurs most frequently wherever the rivers empty into shallow and sheltered bays, as in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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A single consequence is that mountain blocks in many cases are bounded by fault scarps and flexure slopes that descend in stage development to the adjacent lowlands.