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  2. Continental shelf - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf

    The shelf usually ends at a point of increasing slope [3] (called the shelf break). The sea floor below the break is the continental slope. [4] Below the slope is the continental rise, which finally merges into the deep ocean floor, the abyssal plain. [5] The continental shelf and the slope are part of the continental margin. [6]

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    AOL Mail offers a secure and user-friendly email service with spam protection, folders, keyboard shortcuts and more.

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