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The best approximation of the true outer boundary of the continents is the seaward edge of a. continental shelf. b. mid-ocean ridge. c. present-day shorelines. d. ocean trenches.

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The steep rolling submerged surface stretching from the ocean is known as the continental shelf.

Along certain oceans, the shelf is essentially non-existent, however, along other coastlines, the shelf may extend as far as 1500 kilometers out to sea.

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