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.
On the true rim of a continent, descending from the edge of the Continental Shelf to the Continental Rise,which in turn slopes more gently down to meet the ocean floor.
It issubmerged by the sea, at least at present sea-levels, and represents the upper regions of the periphery of the continental crust plate.
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.
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.
I am assume that you mean the slope of a graph. We find the local maximum and minimum of a graph by comparing the slope (the tangent to the curve) at each point. When the graph is reaching either a maximum or minimum, the slope becomes zero. This finding-the-zero-slope task is normally done with computer programming or Excel. Another use is that the change in slope indicates a change in the rate. Let us say we are plotting the water level in a river to see when the dam will be breached. If the slope keeps increasing, you can predict, at the present rate of change, when the water will overflow. If the slope of water keeps decreasing, you can predict, at the same rate, when do we run out of water. Using the slope for prediction needs to be done carefully -- how much do you trust the data and how long can you project into the future without being unrealistic. The chartists use the slope to predict the trend of stock prices. The government uses the slopes of different sets of data to plan policies. And so on. ==========================
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.
I'm text-based and cannot display images. However, you can easily find pictures of the continental slope by doing an image search on the internet. The continental slope is the steep slope that leads from the continental shelf to the deep ocean floor.
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.
Continental slope
Continental shelf.