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  2. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. [1] Although most submarine volcanoes are located in the depths of seas and oceans, some also exist in shallow water, and these can discharge material into the atmosphere during an eruption.

  3. Hydrothermal vent - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_vent

    Oceanographers are studying the volcanoes and hydrothermal vents of the Juan de Fuca mid ocean ridge where tectonic plates are moving away from each other. [105] Hydrothermal vents and other geothermal manifestations are currently being explored in the Bahía de Concepción, Baja California Sur, Mexico. [106]

  4. Tamu Massif - Wikipedia

    en.wikipedia.org/wiki/Tamu_Massif

    In 2015, researchers found that the volcano's structure bore patterns of magnetic striping on either side, indicating that the volcano is likely a hybrid of a mid-ocean ridge and a shield volcano. Geologic data also indicated that Tamu Massif formed at the junction of three mid-ocean ridges, which was a highly unusual occurrence. [14]

  5. List of submarine volcanoes - Wikipedia

    en.wikipedia.org/wiki/List_of_submarine_volcanoes

    A list of active and extinct submarine volcanoes and seamounts located under the world's oceans. There are estimated to be 40,000 to 55,000 seamounts in the global oceans. [ 1 ] Almost all are not well-mapped and many may not have been identified at all.

  6. Undersea mountain range - Wikipedia

    en.wikipedia.org/wiki/Undersea_mountain_range

    In contrast, if formed by past above-water volcanism, they are known as a seamount chain. The largest and best known undersea mountain range is a mid-ocean ridge, the Mid-Atlantic Ridge . [ 1 ] It has been observed that, "similar to those on land, the undersea mountain ranges are the loci of frequent volcanic and earthquake activity".

  7. Lost City Hydrothermal Field - Wikipedia

    en.wikipedia.org/wiki/Lost_City_Hydrothermal_Field

    Lost City is located in the North Atlantic Ocean on the seafloor mountain Atlantis Massif, which is approximately the size of Mount Rainier. [24] The site is described as a long-lived vent field, estimated to be older than 120,000 years by radiocarbon dating the oldest chimney deposits of the field. [ 1 ]

  8. Davidson Seamount - Wikipedia

    en.wikipedia.org/wiki/Davidson_Seamount

    A seamount is an underwater volcano; Davidson rises 7,480 ft (2,280 m) above the surrounding ocean floor. Although there are over 30,000 seamounts in the Pacific Ocean alone, only about 0.1% of them have been explored. [4] The aqueous environment of the seamount means that it behaves differently from volcanoes on land.

  9. Subaqueous volcano - Wikipedia

    en.wikipedia.org/wiki/Subaqueous_volcano

    A subaqueous volcano is a volcano formed from the eruption or flow of magma that occurs under water (as opposed to a subaerial volcanic eruption). [1] Subaqueous volcanic eruptions are significantly more abundant than subaerial eruptions and are estimated to be responsible for 85% of global volcanism by volume.