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  2. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    Submarine volcanoes are underwater vents or fissures in the Earth 's surface from which magma can erupt. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. [1]

  3. Hawaiian eruption - Wikipedia

    en.wikipedia.org/wiki/Hawaiian_eruption

    Hawaiian eruption. A Hawaiian eruption is a type of volcanic eruption where lava flows from the vent in a relatively gentle, low level eruption; it is so named because it is characteristic of Hawaiian volcanoes. Typically they are effusive eruptions, with basaltic magmas of low viscosity, low content of gases, and high temperature at the vent.

  4. Mount Cleveland (Alaska) - Wikipedia

    en.wikipedia.org/wiki/Mount_Cleveland_(Alaska)

    Mount Cleveland is located 490 km (304 mi) from the western end of the Aleutian Arc, [4] a long volcanic chain extending off the coast of Alaska. Containing over 75 volcanoes, [5] this volcanic arc occurs above the subduction zone where the Pacific Plate plunges under the North American Plate.

  5. A (sailing yacht) - Wikipedia

    en.wikipedia.org/wiki/A_(sailing_yacht)

    Cruising: 16 knots (30 km/h) Top: 21 knots (39 km/h) Range. 5,340 nmi (9,890 km) Crew. 54. Sailing Yacht A is a sailing yacht launched in 2015. [2] The vessel is a sail-assisted motor yacht [3] designed by Philippe Starck (exteriors and interiors) [4][5] and built by Nobiskrug in Kiel, Germany for the Russian billionaire Andrey Melnichenko. [6]

  6. 1902 eruption of Mount Pelée - Wikipedia

    en.wikipedia.org/wiki/1902_eruption_of_Mount_Pelée

    The tsunamis swept along the coast, damaging buildings and boats. The explosions resumed the night of 5 May. The following morning, parts of the eruption plume became incandescent, signifying that the character of the eruption had changed. The phreatic eruptions had finally given way to magmatic eruptions as magma reached the surface. These ...

  7. Magma chamber - Wikipedia

    en.wikipedia.org/wiki/Magma_chamber

    A magma chamber is a large pool of liquid rock beneath the surface of the Earth. The molten rock, or magma, in such a chamber is less dense than the surrounding country rock, which produces buoyant forces on the magma that tend to drive it upwards. [1] If the magma finds a path to the surface, then the result will be a volcanic eruption ...

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