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.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
Non-examples of slope include horizontal lines, which have a slope of zero, and vertical lines, which have an undefined slope. Additionally, a constant function, represented by a flat line, also does not demonstrate slope since it does not change in the y-value as the x-value changes. Finally, any situation where there is no change in y despite a change in x does not represent a slope.
two, one is the resultant weight on the slope and = cosine (slope angle) * mass two is the force on the object and acts parralel to the the slope and = sin (slope angle) * mass
The slope of the speed/time graph is the magnitude (size) of the object's acceleration.
continental slope
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
The continental shelf starts from the shore to a few miles out with less gradient of slope. The continental slope starts after shelf-break with a higher slope gradient, then follows the continental rise and abyssal-plain.
A sharp drop-off beyond the continental shelf is called a continental slope. The continental slope marks the transition between the continental shelf and the deep ocean floor.
A continental margin is NOT a part of a continent. It is the submerged outer edge of a continent that includes the continental shelf, continental slope, and continental rise.
continental margin
The continental shelf is a flattish area which extends from the shore out into the ocean and is made of continental crust. This ends in a slope (the continental slope) which descends to the abyssal plane, which is made of oceanic crust.
Abrasion
continental rise
Continental shelf.