Coalescing alluvial fanscone-formed deposits of alluvium that operate alongside one anotherare shaped in which rivers emerge within the mountains. If the rivers are big enough to increase their programs to The ocean, lower deltaic plains build before the enthusiasts; this occurs most often exactly where the rivers vacant into shallow and sheltered bays, as inside the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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One consequence is that mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in step formation into the adjacent lowlands.