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  2. 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 ...

  3. Yellowstone Caldera - Wikipedia

    en.wikipedia.org/wiki/Yellowstone_Caldera

    The Yellowstone Caldera, sometimes referred to as the Yellowstone Supervolcano, is a volcanic caldera and supervolcano in Yellowstone National Park in the Western United States. The caldera and most of the park are located in the northwest corner of the state of Wyoming. The caldera measures 43 by 28 miles (70 by 45 kilometers), and postcaldera ...

  4. Plutonism - Wikipedia

    en.wikipedia.org/wiki/Plutonism

    Plutonism is the geologic theory that the igneous rocks forming the Earth originated from intrusive magmatic activity, with a continuing gradual process of weathering and erosion wearing away rocks, which were then deposited on the sea bed, re-formed into layers of sedimentary rock by heat and pressure, and raised again.

  5. File:Volcano scheme.svg - Wikipedia

    en.wikipedia.org/wiki/File:Volcano_scheme.svg

    File:Volcano scheme.svg. Size of this PNG preview of this SVG file: 573 × 599 pixels. Other resolutions: 230 × 240 pixels | 459 × 480 pixels | 735 × 768 pixels | 979 × 1,024 pixels | 1,959 × 2,048 pixels | 1,099 × 1,149 pixels. This is a file from the Wikimedia Commons. Information from its description page there is shown below.

  6. Peléan eruption - Wikipedia

    en.wikipedia.org/wiki/Peléan_eruption

    Peléan eruptions are a type of volcanic eruption. They can occur when viscous magma, typically of rhyolitic or andesitic type, is involved, and share some similarities with Vulcanian eruptions. The most important characteristic of a Peléan eruption is the presence of a glowing avalanche of hot volcanic ash, called a pyroclastic flow.

  7. Surtseyan eruption - Wikipedia

    en.wikipedia.org/wiki/Surtseyan_eruption

    Surtseyan eruption: 1 water vapor cloud, 2 cypressoid ash jet, 3 crater, 4 water, 5 layers of lava and ash, 6 stratum, 7 magma conduit, 8 magma chamber, 9 dike A Surtseyan eruption is an explosive style of volcanic eruption that takes place in shallow seas or lakes when rapidly rising and fragmenting hot magma interacts explosively with water ...

  8. Thrihnukagigur - Wikipedia

    en.wikipedia.org/wiki/Thrihnukagigur

    The magma that would normally fill the chamber and become sealed is believed to have drained away, to the bewilderment of scientists, revealing the rift beneath the surface. [4] In August 2015, the members of the Icelandic band Kaleo and fourteen support staff descended into the volcano's magma chamber and recorded a live rendition of the band ...

  9. Caldera - Wikipedia

    en.wikipedia.org/wiki/Caldera

    A caldera (/ kɔːlˈdɛrə, kæl -/ [ 1 ]kawl-DERR-ə, kal-) is a large cauldron -like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the structural integrity of such a chamber, greatly ...