Submarine canyons are features associated principally with the continental slope; some are associated with past or present rivers.

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Submarine canyons are features associated with the continental slope, which is the steep gradient that leads from the continental shelf to the deep ocean basin. While some submarine canyons may have been influenced by past or present rivers, they are primarily shaped by other processes such as turbidity currents and erosion from ocean currents.

Submarine Canyons Are Features Associated Principally with the Continental Slope;