Explanation of the continental slope, its steep gradient, and its role in connecting the shallow shelf to the deep ocean floor.
Why Oceans Don't Drain Into the Ground
The Continental Shelf and Slope
The Continental Slope: The Drop-Off
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At the edge of the shelf, the terrain changes abruptly. This is the continental slope. It plunges downward at a much steeper angle than the shelf, reaching depths of thousands of meters. While it looks like a cliff face underwater, it is still made of solid rock. It serves as a bridge between the shallow edges of the continents and the vast, flat abyssal plains of the deep ocean.
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