Coalescing alluvial followerscone-formed deposits of alluvium that operate jointlyare shaped where rivers arise through the mountains. Once the rivers are large plenty of to extend their courses to The ocean, reduced deltaic plains establish in front of the fans; this happens most frequently where by the rivers empty into shallow and sheltered bays, as in 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.