Coalescing alluvial loverscone-shaped deposits of alluvium that run togetherare fashioned the place rivers emerge from the mountains. In the event the rivers are huge sufficient to increase their programs to the sea, very low deltaic plains build before the enthusiasts; this occurs most often in which the rivers vacant into shallow and sheltered bays, as while in the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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1 consequence is the fact that mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in stage formation to the adjacent lowlands.