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Volcano, Planetary

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Encyclopedia of Astrobiology

Definition

Volcanoes are structures (constructional volcano edifices) created by the accumulation of erupted molten lava or solid, fragmental pyroclastic rocks (or pyroclasts). Volcanoes range in size from small cones a few tens of meters high to enormous shields hundreds of km in diameter. Most volcanoes on Earth and other planets are cone shaped. The morphology of the volcano edifice depends basically on the type of volcanic material which erupted. When the lava is relatively fluid, such as basalt, volcanic edifice has slow-angle slopes creating a so-called shield volcano. When the lava consists of very viscous rhyolite, the extrusion of pasty lava tends to form a dome, or the explosive eruption of the highly viscous material and fragmental material will form a steep-sided structure called stratovolcano. Volcanoes are commonly present on Earth as a result of plate tectonicsprocesses and on other telluric planets of our Solar system, namely Mars and Venus, and on Jupiter moon Io....

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References and Further Reading

  • Geissler P (2015) Chapter 44 – Cryovolcanism in the outer solar system. In: Sigurdsson H (ed) The encyclopedia of volcanoes, 2nd edn. Academic, Amsterdam, pp 763–776

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  • Hargitai H, Kereszturi Á, Choukroun M (2014) Cryovolcanic features. In: Hargitai H, Kereszturi Á (eds) Encyclopedia of planetary landforms. Springer, New York, pp 1–10

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Correspondence to Daniele L. Pinti .

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Pinti, D.L. (2022). Volcano, Planetary. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1671-5

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_1671-5

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  • Print ISBN: 978-3-642-27833-4

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Chapter history

  1. Latest

    Volcano, Planetary
    Published:
    27 December 2022

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1671-5

  2. Original

    Volcano
    Published:
    05 May 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1671-4