The edge is called the shelf break. The actual declining shelf is called the called the continental slope.
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
It is called the Continental Shelf
The steep side of the edge of a continent is called a continental slope. This feature marks the transition between the continental shelf and the deep ocean floor.
Continental slope
The continental rise.
Rise
the continental slope
The tip of the continental shelf (which has a gentle slope) where if you go any farther, the continental slope forms, which has a very steep slope.
falseeeeeeeeeeee!!!!!!!!!
The continental slope is the area between the offshore shallows out to where the continental shelf dips steeply to the sea floor. It connects those two areas. The continental shelf is where the shallow waters of the ocean meet the shore. Farther out, the water gets progressively deeper, and this is the continental slope. At the outer edge of the continental slope, the bottom drops sharply away and plunges to the deep ocean. The Wikipedia article has more information and some drawings and diagrams. A link is provided. The steep slopingpart of the ocean floor termination of continental shelves is called continental slope.
False a steep shelf slows the surge. while a slopping shelf will let the water flow.
falseeeeeeeeeeee!!!!!!!!!