Hostname: page-component-78c5997874-m6dg7 Total loading time: 0 Render date: 2024-11-06T15:48:22.536Z Has data issue: false hasContentIssue false
  • English
  • Français

The Surtsey eruption and related scientific work

Published online by Cambridge University Press:  27 October 2009

S. Thorarinsson
Get access Rights & Permissions [Opens in a new window]

Extract

The course of events of the volcanic activity in Surtsey and the adjacent area can be divided into seven main phases:

Submarine phase I

This phase probably started about 6 November 1963, in a fissure, 130 m deep, running N 35° E to S 35° W, in lat 63° 18′ 22″ N, long 20° 36′ 5″ W, 3 nautical miles west-south-west of Geirfuglasker, the southernmost of the Vestmannaeyjar (Fig. 1) The seismograph at Kirkjubæjarklaustur registered weak earthquakes in this area from 6 to 8 November. During the following week submarine action built up a narrow ridge, presumably mainly consisting of pillow lava, near the bottom of the sea floor, and an increasing amount of hyaloclastites as the ridge came nearer the surface.

Type
Articles
Information
Polar Record , Volume 13 , Issue 86 , May 1967 , pp. 571 - 578
Copyright
Copyright © Cambridge University Press 1967

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Selected bibliography

Anderson, R. et al. Electricity in volcanic clouds. Science, Vol. 148, No. 3674, 1965, p. 1179–89.CrossRefGoogle ScholarPubMed
Einarsson, E.The eruption in Surtsey in words and pictures. Heimskringla, Reykjavík, 1966; [Also in Icelandic, German and Danish.].Google Scholar
Fridriksson, S.Um adflutning lífvera til Surtseyjar [The colonization of dry land biota on the island of Surtsey]. Náttúrufrædingurinn, vol 34, No 2, 1965, p 83–89.Google Scholar
Kjartnasson, G. 1966. Stapakenningin og Surtsey [A comparison of table mountains in Iceland and the volcanic island of Surtsey] Natturufrædingurinn, Vol 36, No 1 p 1–34.Google Scholar
Sigurgeirsson, , Th. Jardedlisfrædirannsóknir í sambandi vid Surtseyjargosid [Geophysical research in connection with the volcanic eruption in Surtsey]. Náttúrufrædingurinn, Vol 35, No 4, 1965, p 188–206.Google Scholar
Stefánsson, U.Influence of ths Surtsey eruption on the nutrient content of the surrounding seawater. Sears Foundation: Journal of Marine Research, Vol 24, No 2, 1966, p 141–268.Google Scholar
Surtsey Research Society. Surtsey Research Progress Report No 1. The Surtsey Research Society, Reykjavík (mimeo), 1965.Google Scholar
Surtsey Research Society. Surtsey Research Progress Report No 2. The Surtsey Research Society. Reykjavík (mimeo), 1966.Google Scholar
Thorarinsson, S., Einarsson, Th., Sigvaldason, G. and Elisson, G.The submarine eruption off the Vestmann Islands, 1963–64. Bulletin Volcanologique, (Naples), Vol 27, 1964. p 435–45.CrossRefGoogle Scholar
Thorarinsson, S. and Vonnegut, B.Whirlwinds produced by the eruption of Surtsey volcano. Bulletin of the American Meteorological Society, Vol 45, No 8, 1964, p 440–44.CrossRefGoogle Scholar
Thorarinsson, S.Surtsey: island born of fire. National Geographic Magazine, Vol 127, No 5, 1965, p 712–26.Google Scholar
Thorarinsson, S.Sitt af hverju um Surtseyjargosid [Some facts about the Surtsey eruption]. Náttúrufrædingurinn, Vol 35, No 4, 1965, p 153–81.Google Scholar
Thorarinsson, S.Surtsey. The new island in the North Atlantic. Reykjvík Almenna Bókafélagid, 1964. and New York, Viking Press, 1967 [Also in German, Danish and Swedish].Google Scholar