continental rise

The continental rise is a part of the ocean floor that lies between the continental slope and the deep ocean floor. It forms from sediments that accumulate as they cascade down from the continental shelf above, creating a gently sloping area. This region plays a crucial role in marine sedimentation, acting as a buffer for materials being transported from land to the ocean. The continental rise is important for understanding tectonic activity, ocean currents, and marine ecosystems, as it influences the distribution of nutrients and habitats for various sea life.