The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective

The Eldfell eruption commenced on 23 January 1973 as a 1.5 km fissure crossing the island of Heimaey. Many houses close to the main vent were destroyed by pyroclasts before a flank collapse of the volcano in February allowed lava to move into the town. The Icelanders responded by spraying seawater o...

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Main Author: Morgan, Alan V.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Association of Canada 2000
Subjects:
Online Access:https://journals.lib.unb.ca/index.php/GC/article/view/4030
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spelling ftuninewbrunojs:oai:ojs.journals.lib.unb.ca:article/4030 2023-05-15T16:33:58+02:00 The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective Morgan, Alan V. 2000-03-03 application/pdf https://journals.lib.unb.ca/index.php/GC/article/view/4030 eng eng Geological Association of Canada https://journals.lib.unb.ca/index.php/GC/article/view/4030/4544 https://journals.lib.unb.ca/index.php/GC/article/view/4030 Copyright (c) 2015 Geoscience Canada Geoscience Canada; Volume 27, Number 1 (2000) 1911-4850 0315-0941 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 2000 ftuninewbrunojs 2022-07-11T11:48:03Z The Eldfell eruption commenced on 23 January 1973 as a 1.5 km fissure crossing the island of Heimaey. Many houses close to the main vent were destroyed by pyroclasts before a flank collapse of the volcano in February allowed lava to move into the town. The Icelanders responded by spraying seawater on the lava, finally stopping the advance less than 100 m from the port quay sides. During the eruption period, which lasted until early June, more than 400 establishments were destroyed by tephra fall and lava. The residents of Vestmannaeyjar (~5300 persons at the start of the eruption) were safely evacuated by trawlers and an airlift. Today (1999) the town has approximately 4800 inhabitants, and a thriving post-eruption economy. Résumé La première manifestation de l'éruptiondu volcan Eldfell a été l'apparition d'une fissure de 1,5 km de longueur en travers de l'île de Heimaey. De nombreuses maisons situées à proximité du principal évent ont été détruites par des projections de pyroclastes avant que l'effondrement d'un flanc du volcan en février ne permette à la lave d'envahir la ville. En arrosant le front de laves avec de l'eau de mer, les Islandais ont réussi à stopper la poussée de lave à moins de 100 m des quais. Durant la période d'éruption qui aduré jusqu'en juin 1973, plus de 400 bâtiments ont été détruits par des laves et des projections volcaniques. Les résidents de Vestmannaeyjar (environ 5 300 personnes au début de l'éruption) ont été évacués par chalutiers et par pont aérien. Aujourd'hui (1999), la ville compte 4 800 habitants et son économie est florissante. Article in Journal/Newspaper Heimaey Iceland Vestmannaeyjar University of New Brunswick: Centre for Digital Scholarship Journals Heimaey ENVELOPE(-22.486,-22.486,65.099,65.099) Vestmannaeyjar ENVELOPE(-20.391,-20.391,63.362,63.362) Eldfell ENVELOPE(-20.250,-20.250,63.433,63.433)
institution Open Polar
collection University of New Brunswick: Centre for Digital Scholarship Journals
op_collection_id ftuninewbrunojs
language English
description The Eldfell eruption commenced on 23 January 1973 as a 1.5 km fissure crossing the island of Heimaey. Many houses close to the main vent were destroyed by pyroclasts before a flank collapse of the volcano in February allowed lava to move into the town. The Icelanders responded by spraying seawater on the lava, finally stopping the advance less than 100 m from the port quay sides. During the eruption period, which lasted until early June, more than 400 establishments were destroyed by tephra fall and lava. The residents of Vestmannaeyjar (~5300 persons at the start of the eruption) were safely evacuated by trawlers and an airlift. Today (1999) the town has approximately 4800 inhabitants, and a thriving post-eruption economy. Résumé La première manifestation de l'éruptiondu volcan Eldfell a été l'apparition d'une fissure de 1,5 km de longueur en travers de l'île de Heimaey. De nombreuses maisons situées à proximité du principal évent ont été détruites par des projections de pyroclastes avant que l'effondrement d'un flanc du volcan en février ne permette à la lave d'envahir la ville. En arrosant le front de laves avec de l'eau de mer, les Islandais ont réussi à stopper la poussée de lave à moins de 100 m des quais. Durant la période d'éruption qui aduré jusqu'en juin 1973, plus de 400 bâtiments ont été détruits par des laves et des projections volcaniques. Les résidents de Vestmannaeyjar (environ 5 300 personnes au début de l'éruption) ont été évacués par chalutiers et par pont aérien. Aujourd'hui (1999), la ville compte 4 800 habitants et son économie est florissante.
format Article in Journal/Newspaper
author Morgan, Alan V.
spellingShingle Morgan, Alan V.
The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
author_facet Morgan, Alan V.
author_sort Morgan, Alan V.
title The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
title_short The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
title_full The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
title_fullStr The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
title_full_unstemmed The Eldfell Eruption, Heimaey, Iceland: A 25-Year Retrospective
title_sort eldfell eruption, heimaey, iceland: a 25-year retrospective
publisher Geological Association of Canada
publishDate 2000
url https://journals.lib.unb.ca/index.php/GC/article/view/4030
long_lat ENVELOPE(-22.486,-22.486,65.099,65.099)
ENVELOPE(-20.391,-20.391,63.362,63.362)
ENVELOPE(-20.250,-20.250,63.433,63.433)
geographic Heimaey
Vestmannaeyjar
Eldfell
geographic_facet Heimaey
Vestmannaeyjar
Eldfell
genre Heimaey
Iceland
Vestmannaeyjar
genre_facet Heimaey
Iceland
Vestmannaeyjar
op_source Geoscience Canada; Volume 27, Number 1 (2000)
1911-4850
0315-0941
op_relation https://journals.lib.unb.ca/index.php/GC/article/view/4030/4544
https://journals.lib.unb.ca/index.php/GC/article/view/4030
op_rights Copyright (c) 2015 Geoscience Canada
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