Coalescing alluvial fanscone-formed deposits of alluvium that operate collectivelyare fashioned exactly where rivers arise with the mountains. Once the rivers are large ample to increase their courses to the sea, lower deltaic plains establish in front of the supporters; this happens most often where by the rivers empty into shallow and sheltered bays, as during the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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One consequence is the fact that mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in stage formation into the adjacent lowlands.