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  2. Continental shelf - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf

    The shelves make up less than 10% of the ocean, and a rough estimate suggests that only about 30% of the continental shelf sea floor receives enough sunlight to allow benthic photosynthesis. [36] Though the shelves are usually fertile, if anoxic conditions prevail during sedimentation, the deposits may over geologic time become sources for ...

  3. Scientists looked deep beneath the Doomsday Glacier. What ...

    www.aol.com/news/scientists-looked-deep-beneath...

    Scientists using ice-breaking ships and underwater robots have found the Thwaites Glacier is melting at an accelerating rate and could be on an irreversible path to collapse.

  4. Ross Ice Shelf - Wikipedia

    en.wikipedia.org/wiki/Ross_Ice_Shelf

    The Ross Ice Shelf is one of many such shelves. It reaches into Antarctica from the north, and covers an area of about 520,000 km 2 (200,000 sq mi), nearly the size of France. [2][3] The ice mass is about 800 km (500 mi) wide and 970 km (600 mi) long. In some places, namely its southern areas, the ice shelf can be almost 750 m (2,450 ft) thick.

  5. Continental shelf of the United States - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf_of_the...

    The continental shelf of the United States is one of the largest examples of marine geology in the world, with thousands of miles of submarine land making up the various shelves of the collective. Each different shelf features different extents of continental shelves, from the long, elevated shelves of Alaska, to the short shelf of the Pacific ...

  6. Larsen Ice Shelf - Wikipedia

    en.wikipedia.org/wiki/Larsen_Ice_Shelf

    The Larsen Ice Shelf is a long ice shelf in the northwest part of the Weddell Sea, extending along the east coast of the Antarctic Peninsula [1] from Cape Longing to Smith Peninsula. It is named after Captain Carl Anton Larsen , the master of the Norwegian whaling vessel Jason , who sailed along the ice front as far as 68°10' South during ...

  7. Continental margin - Wikipedia

    en.wikipedia.org/wiki/Continental_margin

    The width of continental shelves worldwide varies in the range of 0.03–1500 km. [4] The continental shelf is generally flat, and ends at the shelf break, where there is a drastic increase in slope angle: The mean angle of continental shelves worldwide is 0° 07′, and typically steeper closer to the coastline than it is near the shelf break. [5]

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