Coalescing alluvial followerscone-shaped deposits of alluvium that operate collectivelyare formed in which rivers arise from your mountains. In the event the rivers are huge ample to extend their classes to the sea, low deltaic plains acquire in front of the fans; this happens most frequently wherever 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 that mountain blocks tend to be bounded by fault scarps and flexure slopes that descend in stage formation to the adjacent lowlands.