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  2. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    The total number of submarine volcanoes is estimated to be over one million (most are now extinct) of which some 75,000 rise more than 1 kilometre (0.62 miles) above the seabed. [1] Only 119 submarine volcanoes in Earth's oceans and seas are known to have erupted during the last 11,700 years. [2] [3]

  3. 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]

  4. 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. Most are unnamed and unexplored.

  5. 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.

  6. Submarine eruption - Wikipedia

    en.wikipedia.org/wiki/Submarine_eruption

    An example is Fukuto-Okanoba near Japan. This activity has been observed for almost a century and causes discoloured water, jets of steam and ash, and pumice is found floating in the surrounding water. [9] Shallow eruptions can lead to the creation of islands. The most well known is Surtsey in Iceland (1963-1967). [10]

  7. Niuafoʻou - Wikipedia

    en.wikipedia.org/wiki/Niuafoʻou

    Niuafoʻou is a volcano located on an underwater ridge 190 kilometres (120 mi) west of the line along which all the other volcanoes of Tonga are ranged. The island contains a steep-sided caldera; its rim is over 120 metres (390 ft) high. It rises to a height of 250 metres (820 ft) at Mokotu.

  8. 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".

  9. Ahyi Seamount - Wikipedia

    en.wikipedia.org/wiki/Ahyi_Seamount

    Ahyi is a submarine volcano which can be found in the northern portion of the Mariana Arc. The structure of the volcano consists of a 12 km (7 mi)-wide stratovolcanic cone that rises from around 2,000 m (6,562 ft) depth to 75 m (246 ft).