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  2. Volcanism - Wikipedia

    en.wikipedia.org/wiki/Volcanism

    Viscous lavas form short, stubby glass-rich flows. These usually have a wavy solidified surface texture. [3] More fluid lavas have solidified surface textures that volcanologists classify into four types. [3] Pillow lava forms when a trigger, often lava making contact with water, causes a lava flow to cool rapidly.

  3. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    A hotspot volcano is center. [8] Movements of tectonic plates create volcanoes along the plate boundaries, which erupt and form mountains. A volcanic arc system is a series of volcanoes that form near a subduction zone where the crust of a sinking oceanic plate melts and drags water down with the subducting crust. [9]

  4. 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.

  5. Volcanic arc - Wikipedia

    en.wikipedia.org/wiki/Volcanic_arc

    The magma ascends to form an arc of volcanoes parallel to the subduction zone. Volcanic arcs are distinct from volcanic chains formed over hotspots in the middle of a tectonic plate. Volcanoes often form one after another as the plate moves over the hotspot, and so the volcanoes progress in age from one end of the chain to the other.

  6. Volcanology - Wikipedia

    en.wikipedia.org/wiki/Volcanology

    The Greek philosopher Empedocles (c. 490-430 BCE) saw the world divided into four elemental forces, of Earth, Air, Fire and Water. Volcanoes, Empedocles maintained, were the manifestation of Elemental Fire. Plato contended that channels of hot and cold waters flow in inexhaustible quantities through subterranean rivers.

  7. Subglacial volcano - Wikipedia

    en.wikipedia.org/wiki/Subglacial_volcano

    During the eruption, the heat of the lava from the subglacial volcano melts the overlying ice. The water quickly cools the lava, resulting in pillow lava shapes similar to those of underwater volcanoes. When the pillow lavas break off and roll down the volcano slopes, pillow breccia, tuff breccia, and hyaloclastite form.

  8. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    The presence of water can greatly alter the characteristics of a volcanic eruption and the explosions of underwater volcanoes in comparison to those on land. For instance, water causes magma to cool and solidify much more quickly than in a terrestrial eruption, often turning it into volcanic glass. The shapes and textures of lava formed by ...

  9. Subaqueous volcano - Wikipedia

    en.wikipedia.org/wiki/Subaqueous_volcano

    A subaqueous volcano is a volcano formed from the eruption or flow of magma that occurs under water (as opposed to a subaerial volcanic eruption). [1] Subaqueous volcanic eruptions are significantly more abundant than subaerial eruptions and are estimated to be responsible for 85% of global volcanism by volume.