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  2. Volcanology - Wikipedia

    en.wikipedia.org/wiki/Volcanology

    In 1841, the first volcanological observatory, the Vesuvius Observatory, was founded in the Kingdom of the Two Sicilies. [1] Volcanology advances have required more than just structured observation, and the science relies upon the understanding and integration of knowledge in many fields including geology, tectonics, physics, chemistry and ...

  3. Volcanism - Wikipedia

    en.wikipedia.org/wiki/Volcanism

    Volcanism on outer solar system moons is powered mainly by tidal heating. [1] Tidal heating caused by the deformation of a body's shape due to mutual gravitational attraction, which generates heat. Earth experiences tidal heating from the Moon, deforming by up to 1 metre (3 feet), but this does not make up a major portion of Earth's total heat. [4]

  4. Plate theory (volcanism) - Wikipedia

    en.wikipedia.org/wiki/Plate_theory_(volcanism)

    [1] The plate theory is a model of volcanism that attributes all volcanic activity on Earth, even that which appears superficially to be anomalous, to the operation of plate tectonics . According to the plate theory, the principal cause of volcanism is extension of the lithosphere .

  5. Volcano - Wikipedia

    en.wikipedia.org/wiki/Volcano

    Augustine Volcano (Alaska) during its eruptive phase on January 24, 2006. A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

  6. Volcanologist - Wikipedia

    en.wikipedia.org/wiki/Volcanologist

    A volcanologist, or volcano scientist, is a geologist who focuses on understanding the formation and eruptive activity of volcanoes. [1] Volcanologists frequently visit volcanoes, sometimes active ones, to observe and monitor volcanic eruptions, collect eruptive products including tephra (such as ash or pumice), rock and lava samples.

  7. Pyroclastic flow - Wikipedia

    en.wikipedia.org/wiki/Pyroclastic_flow

    Pyroclastic flows sweep down the flanks of Mayon Volcano, Philippines, in 2018. A pyroclastic flow (also known as a pyroclastic density current or a pyroclastic cloud) [1] is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano at average speeds of 100 km/h (30 m/s; 60 mph) but is capable of reaching speeds up to ...

  8. A powerful volcano is erupting. Here’s what that could mean ...

    www.aol.com/news/powerful-volcano-erupting-could...

    - Center for Volcanology and Geological Hazard Mitigation/AFP/Getty Images Some gases from Mount Ruang’s eruptions climbed so high they punched into the stratosphere, the second layer of Earth ...

  9. Ejecta - Wikipedia

    en.wikipedia.org/wiki/Ejecta

    Typically in volcanology, ejecta is a result of explosive eruptions.In an explosive eruption, large amounts of gas are dissolved in extremely viscous lava; this lava froths to the surface until the material is expelled rapidly due to the trapped pressure.