Charles Darwin volcanic field
Topic: Earth
From HandWiki - Reading time: 2 min
Charles Darwin volcanic field is a submarine volcanic field in the Cape Verde islands.
It was discovered by the RRS Charles Darwin.[1]
It lies southwest of Santo Antao island at 3,600 metres (11,800 ft) depth. Two vents are named Tambor and Kolá; the first is 2,500 metres (8,200 ft) wide and 250 metres (820 ft) high while the second is 1,000 metres (3,300 ft) wide and 260 metres (850 ft) deep. Both feature 1 kilometre (0.62 mi) wide pit craters.[2] Other vents are known as Tabanka, Batuku, Mandora, De Saude and Koladera. Vents in the Charles Darwin volcanic field include cones with pahoehoe, pillow lavas, scoria and have erupted basalts with xenoliths.[3] Unusually for volcanoes at such depths, they show evidence of explosive eruptions. Volcanic rocks appear to be 1,000s or 10,000s of years old[1] and there is no evidence of Holocene activity but the volcanic field was active in recent times and seismic swarms have been recorded.[4]
Corals and sponges grow on the volcanoes.[5] Bioluminescent gorgonians have been sampled at the Charles Darwin volcanic field.[6]
References
- ↑ 1.0 1.1 Hansteen, Kwasnitschka & Klügel 2014, p. 19.
- ↑ Kwasnitschka, T.; Devey, C. W.; Hansteen, T. H.; Freundt, A.; Kutterolf, S. (December 2013). "Explosive Volcanic Activity at Extreme Depths: Evidence from the Charles Darwin Volcanic Field, Cape Verdes" (in en). AGUFM 2013: V41D–2843. Bibcode: 2013AGUFM.V41D2843K.
- ↑ Hansteen, Kwasnitschka & Klügel 2014, pp. 22-23.
- ↑ Faria, B.; Fonseca, J. F. B. D. (28 February 2014). "Investigating volcanic hazard in Cape Verde Islands through geophysical monitoring: network description and first results" (in English). Natural Hazards and Earth System Sciences 14 (2): 496. doi:10.5194/nhess-14-485-2014. ISSN 1561-8633. Bibcode: 2014NHESS..14..485F.
- ↑ Hansteen, Kwasnitschka & Klügel 2014, p. 7.
- ↑ Raddatz, Jacek; López Correa, Matthias; Rüggeberg, Andres; Dullo, Wolf-Christian; Hansteen, Thor (September 2011). "Bioluminescence in deep-sea isidid gorgonians from the Cape Verde archipelago" (in en). Coral Reefs 30 (3): 579. doi:10.1007/s00338-011-0743-5. ISSN 0722-4028. Bibcode: 2011CorRe..30..579R.
Sources
- Hansteen, Thor; Kwasnitschka, Tom; Klügel, Andreas (2014). Cape Verde Seamounts - Cruise No. M80/3 - December 29, 2009 - February 1, 2010 - Dakar (Senegal) - Las Palmas de Gran Canaria (Spain) (Report). Bremen. https://www.tib.eu/en/search/id/awi:doi~10.2312%252Fcr_m80_3/Cape-Verde-Seamounts-Cruise-No-M80-3-December-29/.
 |  |
EncycloReader
is supported by the 
KSF