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  2. Lava dome - Wikipedia

    en.wikipedia.org/wiki/Lava_dome

    The former implies the enlargement of a lava dome due to the influx of magma into the dome interior, and the latter refers to discrete lobes of lava emplaced upon the surface of the dome. [2] It is the high viscosity of the lava that prevents it from flowing far from the vent from which it extrudes, creating a dome-like shape of sticky lava ...

  3. Dome (geology) - Wikipedia

    en.wikipedia.org/wiki/Dome_(geology)

    A dome is a feature in structural geology where a circular part of the Earth's surface has been pushed upward, tilting the pre-existing layers of earth away from the center. In technical terms, it consists of symmetrical anticlines that intersect each other at their respective apices .

  4. Cerro Chao - Wikipedia

    en.wikipedia.org/wiki/Cerro_Chao

    The volume of Chao is exceptional for a lava dome structure, although the lava flux rate generating it is low in comparison to a basaltic eruption like Laki in Iceland. This low flux rate is insufficient to cause caldera formation. Cerro Chao is the largest Quaternary silicic lava flow in the world. [1]

  5. Extrusive rock - Wikipedia

    en.wikipedia.org/wiki/Extrusive_rock

    Lava domes are formed by high viscosity lava that piles up, forming a dome shape. Domes typically solidify to form the rich in silica extrusive rock obsidian and sometimes dacite domes form the extrusive rock dacite, like in the case of Mount St. Helens. [2] Calderas are volcanic depressions formed after an erupted volcano collapses.

  6. Lava - Wikipedia

    en.wikipedia.org/wiki/Lava

    Lava domes are formed by the extrusion of viscous felsic magma. They can form prominent rounded protuberances, such as at Valles Caldera. As a volcano extrudes silicic lava, it can form an inflation dome or endogenous dome, gradually building up a large, pillow-like structure which cracks, fissures, and may release cooled chunks of rock and rubble.

  7. Cerro Porquesa - Wikipedia

    en.wikipedia.org/wiki/Cerro_Porquesa

    The lava dome is accompanied by block-and-ash flows and lava flows [5] and the presence of two volcanic cones has been reported. [6] The lava dome is of Pliocene/Pleistocene age [7] with little glacial features on the younger domes indicating young ages. [1] The Quebrada de Piga, which flows to Salar del Huasco, originates at Cerro Porquesa. [8]

  8. Kilauea is spewing lava again. It is the Hawaii volcano's ...

    www.aol.com/kilauea-shooting-lava-again-hawaii...

    Kilauea volcano began shooting lava into the air once again Tuesday on the Big Island of Hawaii. Kilauea, one of the world's most active volcanoes, has been erupting on and off for nearly two ...

  9. List of lava domes - Wikipedia

    en.wikipedia.org/wiki/List_of_lava_domes

    Lava domes are common features on volcanoes around the world. Lava domes are known to exist on plate margins as well as in intra-arc hotspots, and on heights above 6000 m and in the sea floor. [1] Individual lava domes and volcanoes featuring lava domes are listed below.