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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. 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 ...

  4. Kamaʻehuakanaloa Seamount - Wikipedia

    en.wikipedia.org/wiki/Kamaʻehuakanaloa_Seamount

    The top of the seamount is about 3,200 ft (975 m) below sea level. This seamount is on the flank of Mauna Loa, the largest active subaerial shield volcano on Earth. [8] [9] Kamaʻehuakanaloa is the newest volcano in the Hawaiian–Emperor seamount chain, a string of volcanoes that stretches about 3,900 mi (6,200 km) northwest of Kamaʻehuakanaloa.

  5. Mount Tarawera - Wikipedia

    en.wikipedia.org/wiki/Mount_Tarawera

    Mount Tarawera is a volcano on the North Island of New Zealand within the older but volcanically productive Ōkataina Caldera. Located 24 kilometres southeast of Rotorua , it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886 .

  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. Mount Mazama - Wikipedia

    en.wikipedia.org/wiki/Mount_Mazama

    Its collapse, due to the eruption of magma emptying the underlying magma chamber, formed a caldera that holds Crater Lake (Giiwas in the Native American language Klamath). [6] Mount Mazama originally had an elevation of 12,000 feet (3,700 m), but following its climactic eruption this was reduced to 8,157 feet (2,486 m).

  8. Marsili - Wikipedia

    en.wikipedia.org/wiki/Marsili

    Marsili. Aeolian arc, including coastline and depth contour lines for every 500 meters. /  39.25000°N 14.39444°E  / 39.25000; 14.39444. Marsili is a large undersea volcano in the Tyrrhenian Sea, about 175 kilometers (109 mi) south of Naples. The seamount is about 3,000 m (9,800 feet) tall; its peak and crater are about 450 m below the ...

  9. Big Ben (Heard Island) - Wikipedia

    en.wikipedia.org/wiki/Big_Ben_(Heard_Island)

    Big Ben (previously known as Big Ben Peak, Old Ben Mountain, Emperor William Peak and Kaiser Wilhelm-Berg) [1] is a volcanic massif that dominates the geography of Heard Island in the southern Indian Ocean. It is a stratovolcano with a diameter of about 25 km (16 mi). Its highest point is Mawson Peak, which is 2,745 m (9,006 ft) above sea level.

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