The process in which depressions fill up and the level of surface rises
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Continental rise, a major depositional regime in oceans made up of thick sequences of continental material that accumulate between the continental slope and the abyssal plain. Continental rises form as a result of three sedimentary processes: mass wasting, the deposition from contour currents, and the vertical settling of clastic and biogenic particles
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aggradation is the process in which depressions fills up and the level of surface rises.
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