Coalescing alluvial enthusiastscone-formed deposits of alluvium that run togetherare shaped where by rivers emerge through the mountains. When the rivers are huge more than enough to extend their programs to The ocean, low deltaic plains build before the fans; this occurs most often wherever the rivers empty into shallow and sheltered bays, as inside the deltas of Kantō (Kwanto), Nōbi, and Ōsaka.
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One particular consequence is mountain blocks are frequently bounded by fault scarps and flexure slopes that descend in step development to the adjacent lowlands.