At the shoreline
Yes, the continental slope drops downward to the edge of the continent at which point it plummets down for the depth of the continental plate. It depends upon whom you speak with, but a nation's boundary is generally considered 200 miles beyond that.
The world's combined continental slope is about 200,000 mi (300,000 km) long and descends at an average angle of about 4° from the edge of the continental shelf to the beginning of the ocean basins at depths of 330 - 10,500 ft (100 - 3,200 m). The slope is most gradual off stable coasts without major rivers and is steepest off coasts with young mountain ranges and narrow continental shelves. Slopes off mountainous coastlines and narrow shelves commonly have outcrops of rock. The dominant sediments of continental slopes are muds; there are smaller amounts of sediments of sand or gravel.
The "North Slope" refers to the region of the state of Alaska located on the northern slope of the Brooks Range (mountains), along the Arctic Ocean, the Chukchi Sea, and the Beaufort Sea.
then the slope is x=y. there is no slope.
Continental shelf.
The continental rise is located at the base of the continental slope, where the incline lessens and sediment from the continent accumulates. It marks the transition between the continental margin and the deep ocean basin.
There are not many plants that live in the continental slope. One of the few plants that live here is algae.
The accumulation of sediment at the bottom of a continental slope is referred to as continental rise. This phenomenon occurs in oceans throughout the world.
continental slope
The area you are referring to is known as the continental rise. It is located at the base of the continental slope and consists of a thick accumulation of sediments that have been transported down from the continent. The continental rise marks the transition between the continental margin and the deep ocean basin.
The portion of the continental margin that serves as a boundary between the oceanic crust and the continental crust is called the continental shelf. This is the shallowest part of the margin, located between the shoreline and the continental slope.
I'm unable to show you a picture directly, but I can describe the continental slope to you. The continental slope is the steeply sloping transition between the continental shelf and the deep ocean floor. It is typically located at depths of around 200 to 2,000 meters and marks the beginning of the oceanic crust. The slope is often characterized by submarine canyons and sediment deposits as it descends into the abyssal plain.
The continental shelf is basically an extension of a continent into an ocean. It is underwater during interglacial periods (such as today) but dry during glacial periods. The continental slope is the sloping area between the continental shelf and the continental rise (where the continental plate meets the oceanic plate). The continental shelf and the continental slope together are called the continental margin. The continental rise is located at the bottom of the continental slope and is formed by the accumulation of sediment from the continent. Past the continental rise lies the abyssal plain which is the flat ocean floor.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf, continental slope, and continental rise combine to form the continental margin.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench