The processes influence the shape and features of continental shelves are.
Three sedimentary processes combine to produce continental rises: vertical clastic and biogenic particle settling, contour current deposition, and mass wasting.
Ocean currents, sediment buildup, and the presence of a plate boundary are frequently responsible for determining a continental shelf's breadth. The area between the continental shelf and the deep ocean floor is known as a continental slope. The slopes of the continents are typically shaped by sediments.
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