The shelf ends at a break, where the increased steepness is defined as the continental slope.
These landslides either originate in submarine canyons or on the continental slope.
From the break, the shelf descends toward the deep ocean floor in what is called the continental slope.
At the outer edge of the continental shelf, the land drops off sharply in what is called the continental slope.
The features of note are the various canyons, gullies, and channels dissecting the continental slope.
Also note the beautiful submarine valley heading out seaward of the continental slope onto the less-deformed oceanic plate.
The continental shelf extends outward to the continental slope where the deep ocean truly begins.
Sediments on the steep continental slope are mostly soft mud, which is finer than sediments found on the shelf.
At the base of the continental slope, in some areas, a smooth gently sloping apron of sediments merges into the deep-sea floor.
For the case shown above, the earthquake rupture occurred at the base of the continental slope in relatively deep water.
continental slope in Science
continental slope The sloping region between a continental shelf and a continental rise. A continental slope is typically about 20 km (12.4 mi) wide, consists of muds and silts, and is often crosscut by submarine canyons.