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Made of continental crust- Shallower than the deep-ocean basin
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Begins at shoreline and slopes gently down
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Begins at the edge of the shelf and continues down to the flattest part of the ocean floor
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The base of the continental slope, is made of large piles of sediment
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Made of oceanic Crust- deeper than the continental margin
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Mountain chains that form when tectonic plates pull apart. Creates cracks in the ocean floor called RIFT ZONES
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The broad, flat part of the deep-ocean basin
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Huge cracks in the deep-ocean basin
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is the Study of the shape and features of Land Features
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Individual mountains of volcanic material
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Sound Navigation and ranging