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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. Aira Caldera - Wikipedia

    en.wikipedia.org/wiki/Aira_Caldera

    1955 to present. Aira Caldera is a gigantic volcanic caldera that is located on the southern end of Kyushu, Japan. It is believed to have been formed about 30,000 years ago with a succession of pyroclastic surges. [1][2] It is currently the place of residence to over 900,000 people. The shores of Aira Caldera are home to rare flora and fauna ...

  4. Rhyolite - Wikipedia

    en.wikipedia.org/wiki/Rhyolite

    Rhyolite (/ ˈraɪ.əlaɪt / RY-ə-lyte) [1][2][3][4] is the most silica -rich of volcanic rocks. It is generally glassy or fine-grained (aphanitic) in texture, but may be porphyritic, containing larger mineral crystals (phenocrysts) in an otherwise fine-grained groundmass. The mineral assemblage is predominantly quartz, sanidine, and plagioclase.

  5. One of Mongolia’s best-kept secrets looks more like Greece ...

    www.aol.com/one-mongolia-best-kept-secrets...

    At 74 kilometers long, 31 kilometers wide and reaching depths of 80 meters, it’s Mongolia’s third-largest lake. Khetsuu Khad, the main attraction, is a natural rock formation that runs along ...

  6. 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 ...

  7. Hōei eruption - Wikipedia

    en.wikipedia.org/wiki/Hōei_eruption

    The Hōei quake caused stress and compression of the magma chambers underneath Mount Fuji, leading to the eruption. A dike system stretches from the surface of Mount Fuji to 20 km into the subsurface. At 8 km depth, there are magma chambers of a dacitic and andesitic nature while at the deepest portion of the dike, a basaltic melt is located. [4]

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