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  2. Seamount - Wikipedia

    en.wikipedia.org/wiki/Seamount

    A seamount is a large submarine landform that rises from the ocean floor without reaching the water surface (), and thus is not an island, islet, or cliff-rock.Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to 1,000–4,000 m (3,300–13,100 ft) in height.

  3. Wikipedia:WikiProject Seamounts/Images - Wikipedia

    en.wikipedia.org/wiki/Wikipedia:WikiProject...

    Pillow Lava, a type of lava originating from Seamounts. Rosy Rockfish and Strawberry Anemones at 55.5 meters depth, Cordell Bank Benthic octopus and clam on the Davidson Seamount at 1461 meters.

  4. List of volcanoes in the Hawaiian–Emperor seamount chain

    en.wikipedia.org/wiki/List_of_volcanoes_in_the...

    The Hawaiian–Emperor seamount chain is a series of volcanoes and seamounts extending about 6,200 km (3,900 mi) across the Pacific Ocean. [ n 1 ] The chain was produced by the movement of the ocean crust over the HawaiĘ»i hotspot , an upwelling of hot rock from the Earth's mantle .

  5. Hawaiian–Emperor seamount chain - Wikipedia

    en.wikipedia.org/wiki/Hawaiian–Emperor_seamount...

    The Hawaiian–Emperor seamount chain is a mostly undersea mountain range in the Pacific Ocean that reaches above sea level in Hawaii.It is composed of the Hawaiian ridge, consisting of the islands of the Hawaiian chain northwest to Kure Atoll, and the Emperor Seamounts: together they form a vast underwater mountain region of islands and intervening seamounts, atolls, shallows, banks and reefs ...

  6. Cobb–Eickelberg Seamount chain - Wikipedia

    en.wikipedia.org/wiki/Cobb–Eickelberg_Seamount...

    1. Axial Seamount (46° 03′ 36″ N, 130° 00′ 0″ W). The most recent seamount. Axial Seamount is the youngest seamount in the Cobb Eickelberg Seamount chain. Since this is the most active of all the Cobb-Eickelberg Seamounts, it is studied the most: to help understand the dynamics of seamounts, volcanic activity, earthquakes, biodiversity, geology and chemistry.

  7. List of seamounts in the Southern Ocean - Wikipedia

    en.wikipedia.org/wiki/List_of_seamounts_in_the...

    Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to 1,000–4,000 m (3,300–13,100 ft) in height. They are defined by oceanographers as independent features that rise to at least 1,000 m (3,281 ft) above the seafloor, characteristically of conical form.

  8. Underwater mountain twice height of Burj Khalifa discovered ...

    www.aol.com/news/underwater-mountain-twice...

    Seamounts are underwater mountains usually formed from the remnants of extinct volcanoes. The giant structure measures 5,249ft (1,600m), making it twice the height of the Burj Khalifa in the ...

  9. New England Seamounts - Wikipedia

    en.wikipedia.org/wiki/New_England_Seamounts

    The New England Seamounts is a chain of over twenty underwater extinct volcanic mountains known as seamounts. [1] This chain is located off the coast of Massachusetts in the Atlantic Ocean and extends over 1,000 kilometers (600 mi) from the edge of Georges Bank. Many of the peaks of these mountains rise over 4,000 meters (13,000 ft) from the ...