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Flank eruption

Today, Flank eruption is a topic that has acquired great relevance in various areas. From the political to the technological sphere, Flank eruption has captured the attention of millions of people around the world. Its importance lies in its influence on society and the way it impacts our daily lives. Throughout history, Flank eruption has evolved and generated heated debates that have set standards and significant changes in different sectors. In this article, we will explore the many facets of Flank eruption and analyze its impact today.

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The 2002 eruption of Mount Etna was a flank eruption, occurring along two rift zones to the north-east and south of the summit craters. In this image taken from the International Space Station, the northeast flank is in the foreground. Steam rising from the summit craters obscures the lower part of the south flank eruption column.

A flank eruption is a volcanic eruption which occurs on the flanks of a volcano, instead of at its summit. Such eruptions occur when the conduit connecting the summit to the magma chamber below is blocked, forcing the magma to move laterally.

Overview

At some volcanoes, flank eruptions are common, and occur along clearly defined rift zones. This is the case at Mauna Loa and Kilauea volcanoes in Hawaii, Piton de la Fournaise on Réunion Island,[1] and Mount Etna in Italy.[2] Flank and summit eruptions may occur at the same time.[3]

Where there are inhabited areas on the flanks of a volcano, flank eruptions may be more destructive and dangerous than summit eruptions.[4] Flank eruptions may also trigger the collapse of the volcanic edifice, causing lateral eruptions (such as the 1980 eruption of Mount St. Helens), landslides and tsunamis. Collapse-drive eruptions are among the largest and most destructive volcanic phenomena.[5]

References

  1. ^ Michon, Laurent; Ferrazzini, Valérie; Di Muro, Andrea; Villeneuve, Nicolas; Famin, Vincent (September 15, 2015). "Rift zones and magma plumbing system of Piton de la Fournaise volcano: How do they differ from Hawaii and Etna?" (PDF). Journal of Volcanology and Geothermal Research. 303: 112–129. Bibcode:2015JVGR..303..112M. doi:10.1016/j.jvolgeores.2015.07.031.
  2. ^ Bonforte, Alessandro; Fanizza, Giovanni; Greco, Filippo; Matera, Alfredo; Sulpizio, Roberto (September 15, 2017). "Long-term dynamics across a volcanic rift: 21years of microgravity and GPS observations on the southern flank of Mt. Etna volcano". Journal of Volcanology and Geothermal Research. 344: 174–184. Bibcode:2017JVGR..344..174B. doi:10.1016/j.jvolgeores.2017.06.005.
  3. ^ "The 2018 rift eruption and summit collapse of Kīlauea Volcano | Science". science.sciencemag.org. Archived from the original on 2019-01-25.
  4. ^ Negro, Ciro Del; Cappello, Annalisa; Bilotta, Giuseppe; Ganci, Gaetana; Hérault, Alexis; Zago, Vito (2019). "Living at the edge of an active volcano: Risk from lava flows on Mt. Etna". GSA Bulletin. 132 (7–8): 1615–1625. doi:10.1130/B35290.1. S2CID 212809291.
  5. ^ Hunt, James E.; Cassidy, Michael; Talling, Peter J. (January 18, 2018). "Multi-stage volcanic island flank collapses with coeval explosive caldera-forming eruptions". Scientific Reports. 8 (1): 1146. Bibcode:2018NatSR...8.1146H. doi:10.1038/s41598-018-19285-2. PMC 5773679. PMID 29348427.


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