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occurred. As a result of the Cumbre Vieja eruption, over 5,000 of the islandâs inhabitants had to evacuate, significantly decreasing casualties. Still, more than 1300 homes and 1500 utility buildings were damaged and continuous magma flow stalled repair efforts for weeks.
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Carracedo, Juan C.; Troll, Valentin R.; Day, James M. D.; Geiger, Harri; Aulinas, Meritxell; Soler, Vicente; Deegan, Frances M.; PerezâTorrado, Francisco J.; Gisbert, Guillem; Gazel, Esteban; RodriguezâGonzalez, Alejandro; Albert, Helena (2022).
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However, this hypothesis has been scrutinized for periods of up to several million years of a lack of volcanic activity between islands.
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The 2011â2012 submarine eruption off El Hierro, Canary
Islands: New lessons in oceanic island growth and volcanic crisis management
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hypothesis on Canary hotspot formation proposes how the current-day Canary islands rested above a province of
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eruption, the volcano has remained very active, as since
October 2017 until the 2021 eruption alone, nine
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Troll, Valentin R.; Carracedo, Juan Carlos (2016), Troll, Valentin R.; Carracedo, Juan Carlos (eds.),
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on
September 20, 2021, over 25,000 earthquakes were recorded starting on September 10. Since the 1971
83:(CAMP), became active and extended over 10 million km, developing into what scientists call today the
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Carracedo, J.C.; Troll, V.R.; Zaczek, K.; RodrĂguez-GonzĂĄlez, A.; Soler, V.; Deegan, F.M. (2015)
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Negredo, Ana M.; van Hunen, Jeroen; RodrĂguez-GonzĂĄlez, Juan; Fullea, Javier (2022).
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338:"The 2021 eruption of the Cumbre Vieja volcanic ridge on La Palma, Canary Islands"
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234:"On the origin of the Canary Islands: Insights from mantle convection modelling"
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then shifted the plate the archipelago rests on over a stationary mantle plume
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87:. The archipelago formed about 60 million years ago from a magma source. The
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movements beneath the island. This resulted in fears of an imminent
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on the ocean floor. Eruptions continued until March 2012.
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47:. Hypotheses for this volcanic activity include a deep
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eruptions remain the most recent
Canarian eruptions.
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beginning about 70 million years ago. The underwater
215:, Earth-Science Reviews, volume 150, pages 168â200,
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16:Volcanically active region off the coast of Africa
301:"Chapter 1 - The Canary Islands: An Introduction"
39:and volcanically active region centred on the
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108:From July to September 2011, the Canarian
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43:located off the north-western coast of
23:A satellite image of the Canary Islands
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238:Earth and Planetary Science Letters
185:2021 Cumbre Vieja volcanic eruption
743:. You can help Knowledge (XXG) by
313:10.1016/b978-0-12-809663-5.00001-3
81:Central Atlantic Magmatic Province
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305:The Geology of the Canary Islands
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795:Volcanism of the Canary Islands
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120:, believed to be the result of
116:experienced thousands of small
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190:Geology of the Canary Islands
79:. The province, known as the
307:, Elsevier, pp. 1â41,
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259:10.1016/j.epsl.2022.117506
180:2011â12 El Hierro eruption
152:eruption on the island of
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708:Proposed mechanisms:
528:Indo-Australian Plate
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136:Cumbre Vieja eruption
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685:South American Plate
589:North American Plate
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104:El Hierro eruption
85:Mid-Atlantic Ridge
31:, also called the
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800:Volcanology stubs
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322:978-0-12-809663-5
162:earthquake swarms
126:volcanic eruption
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269:10261/344957
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150:Cumbre Vieja
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57:Cumbre Vieja
49:mantle plume
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737:volcanology
607:Yellowstone
561:Nazca Plate
460:New England
75:during the
784:Categories
645:Louisville
480:St. Helena
244:: 117506.
196:References
665:Rarotonga
655:Marquesas
650:Macdonald
574:GalĂĄpagos
551:Lord Howe
546:Tasmantid
518:Jan Mayen
437:Kerguelen
370:246950800
362:0266-6979
286:247968278
278:0012-821X
114:El Hierro
67:The deep
63:Formation
53:El Hierro
698:Trindade
660:Pitcairn
541:Crosgove
411:Hotspots
169:See also
158:TeneguĂa
154:La Palma
693:Noronha
675:Society
602:Bermuda
513:Iceland
485:Tristan
465:RĂ©union
427:Balleny
246:Bibcode
130:fissure
118:tremors
37:hotspot
35:, is a
640:Hawaii
597:Anahim
569:Easter
503:Azores
455:Canary
432:Erebus
368:
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284:
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110:island
45:Africa
735:This
670:Samoa
630:Bowie
625:Arago
508:Eifel
470:Shona
366:S2CID
282:S2CID
122:magma
741:stub
635:Cobb
358:ISSN
317:ISBN
274:ISSN
27:The
350:doi
309:doi
264:hdl
254:doi
242:584
217:doi
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