Magma chamber

11 – magma chamber

A magma chamber is a large pool of liquid rock under the surface of the Earth.

The molten rock, or magma, in such a chamber is less dense than the surrounding rock. This produces buoyant forces on the magma that tend to drive it upwards.

If the magma finds a path to the surface, then the result may be a volcanic eruption. Many volcanoes sit over magma chambers. These chambers are hard to detect if they are deep within the Earth. Most of those known are close to the surface.

References

  1. ↑ Philpotts, Anthony R.; Ague, Jay J. (2009). Principles of igneous and metamorphic petrology (2nd ed.). Cambridge, UK: Cambridge University Press. pp. 28–32. ISBN 9780521880060.
  2. ↑ "Forensic Probe of Bali's Great Volcano". Eos. 12 February 2019. Retrieved 2020-11-25.
  3. ↑ Dahren, Börje; Troll, Valentin R.; Andersson, Ulf B.; Chadwick, Jane P.; Gardner, Màiri F.; Jaxybulatov, Kairly; Koulakov, Ivan (2012-04-01). "Magma plumbing beneath Anak Krakatau volcano, Indonesia: evidence for multiple magma storage regions". Contributions to Mineralogy and Petrology. 163 (4): 631–651. Bibcode:2012CoMP..163..631D. doi:10.1007/s00410-011-0690-8. ISSN 1432-0967. S2CID 52064179.