Heimaey of Iceland An Icelandic tale of fire

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Heimaey of Iceland An Icelandic tale of fire, flows, and Vestmann ingenuity T. Saylor

Heimaey of Iceland An Icelandic tale of fire, flows, and Vestmann ingenuity T. Saylor IV

The Basics � 6 km off the mainland �Last erupted January 1 23, 1973

The Basics � 6 km off the mainland �Last erupted January 1 23, 1973 – Eldfell (Mountain of Fire) �Eruption ended late February of the same year �Island was originally fueled by Submarine volcanism and created by Helgafell �Fishing City �Population of ~ 4, 100 (2011) Fig 1 A

Vestmannaeyjar �Along the Mid-Atlantic Ridge �Youngest volcanic system in Fig 2 A 2 Fig

Vestmannaeyjar �Along the Mid-Atlantic Ridge �Youngest volcanic system in Fig 2 A 2 Fig 2 B the Eastern zone of Icelandic volcanism (Subaerial vents of Holocene age) �Named after original Irish slave settlers �Vestmenn (West men), Aeyjar (Islands) �Most Famous Island, Heimaey �Also home to Surtsey (20 km to the SW)

Early History � Iceland first settled by the Norse Gaells (Ostmann, or East men)

Early History � Iceland first settled by the Norse Gaells (Ostmann, or East men) who brought Irish slaves in 874 (recognized as first settlers) � Hjörleifur, murdered by these slaves in his first year � Ingolfur (3 A), Hjörleifur’s blood brother tracked them down to Heimaey, and enacted revenge � Later, in 1627, the islands were captured by Barbary Pirates from Algiers � Gained modern fame through Surtseys eruption in 1963 (3 B) 3 Fig 3 A Fig 3 B

Icelands Volcanic History �~ 125 volcanic eruptions documented since 874 A. D. (USGS, 1973)

Icelands Volcanic History �~ 125 volcanic eruptions documented since 874 A. D. (USGS, 1973) � 14 offshore eruptions, centered mainly off of the Reykjanes Ridge (USGS, 1973 4 Fig 4 A

Eldfell � 1: 55 AM January 23, Fig 4 A 5 Fig 4 B

Eldfell � 1: 55 AM January 23, Fig 4 A 5 Fig 4 B 1973, 10 years after Surtsey �A 2 km long fissure opened in the ground in what was originally a peaceful field �A vent centralized to the NE and Eldfell was born

6 Fig 6 A

6 Fig 6 A

The Fissure/Cone �Dormant for approximately 5, 000 years � 20 million cubic meters of

The Fissure/Cone �Dormant for approximately 5, 000 years � 20 million cubic meters of tephra ejected �Built the cone in 2 days �Eventually became 183 m tall (February of 1973) Fig 7 B 7 Fig 7 A

Lava! � 230 million cubic meters of lava �Alkali basalt (Murgearite to Hawaiite) �Flow

Lava! � 230 million cubic meters of lava �Alkali basalt (Murgearite to Hawaiite) �Flow rate of 3 -9 meters a day, moving towards the town and harbor, so low effusion rate �Submarine volcanism (Surtseyan), later moved to Hawaaiin �Initial Eruptive rate: 100 m 3/sec �Seawater to the rescue! Fig 8 A 8

Fig 9 A Simmer down now! �Large scale cooling 9 effort �Pumping equipment borrowed

Fig 9 A Simmer down now! �Large scale cooling 9 effort �Pumping equipment borrowed from the U. S. � 1. 5 billion gallons of water � 30 km of pipe � 43 pumps �Began in early July, 1973 �Used bulldozers to move tephra over the Fig 9 B

More on cooling � Workers laying pipes over 10 actively moving flows (10 A)

More on cooling � Workers laying pipes over 10 actively moving flows (10 A) � No casualties during this effort � A few cases of minor burns � The pipe supports quickly burned, but the pipes themselves were still cool due to the seawater moving through them that they survived. These pipes can still be seen today. � Mostly inhabitants who volunteered to stay and help fight the flames as well as a team of Icelandic scientists and engineers (USGS, 1973) � Most ambitious attempt by man to control a volcanic Fig 10 A

After the Eruption � ~350 buildings burnt to 11 the ground � 70 homes

After the Eruption � ~350 buildings burnt to 11 the ground � 70 homes nearly completely buried in tephra � ~ 15 million cubic meters of tephra needed to be removed from the town � Most of the towns original inhabitants returned for the cleanup efforts. Fig 11 A

Geothermal power �Heat was extracted from 12 the slowly cooling lava flows; Fig 12

Geothermal power �Heat was extracted from 12 the slowly cooling lava flows; Fig 12 A shows latent subthermal heat after the 1973 eruption �Used as a heating system for the town of Vestmannaeyjar �System emplaced in 1979 and operated for ten years until the flows cooled. Fig 12 A

Geothermal System Schematic � Fig 13 A; a USGS schematic for the geothermal heating

Geothermal System Schematic � Fig 13 A; a USGS schematic for the geothermal heating system used in Heimaey, Iceland. 13

Heimaey Today Fig 14 B �Approximately 4, 100 inhabitants (2011) �Still Icelands most important

Heimaey Today Fig 14 B �Approximately 4, 100 inhabitants (2011) �Still Icelands most important fishing harbor �For a sweet panorama showing the town today as well as Helgafell and Eldfell, follow this link: http: //www. vestmannaeyjar. pano 3 d. eu/ �Þjóðhátíð, a festival celebrating Icelands independence from Denmark is now the main attraction Heimaey offers; 24 hours of fun and beer! �Also home to Puffins!Fig (Fig 14 A 14 B) 14

Heimaey Hazard Map � Lava and 15 pyroclastics Hazard Map � Proximal hazard �

Heimaey Hazard Map � Lava and 15 pyroclastics Hazard Map � Proximal hazard � Medial Hazard � Distal Hazard � Hazard Maps created by Tom Saylor IV using Google. Eart h, USGS, known weather patterns and other Fig 15 A

Hazard Map Cont. � Tephra and 16 Ejecta Hazard Map � Proximal hazard �

Hazard Map Cont. � Tephra and 16 Ejecta Hazard Map � Proximal hazard � Medial Hazard � Distal Hazard � Hazard Maps created by Tom Saylor IV using Google. Earth, USGS, known weather patterns and other Fig 16 A

A note on the previous Hazard Map � During the 1973 eruption, prevailing winds

A note on the previous Hazard Map � During the 1973 eruption, prevailing winds blew tephra to the North East rather than the South West. � The dominant wind pattern for Heimaey is a South Westerly wind, but depending on time of year as well as other weather conditions this can change (Weather Underground, 2012). � Fig 17 A (USGS, 1973) shows the plume rising from Heimaey during the 1973 eruption. Fig 17 A 17

Volcanic (mostly) Videos �Follow this link for a video of the 1973 eruption and

Volcanic (mostly) Videos �Follow this link for a video of the 1973 eruption and evacuation efforts: http: //www. youtube. com/watch? v=VX 9 e 9 ei 6 v 3 s �Follow this link for an educational video on the 1963 Surtsey eruption and the 1973 eruption of Eldfell: http: //www. youtube. com/watch? v=_s. Rw_e 5 RA 34 �For nearly 30 minutes of uninterrupted Puffin action, follow this link: http: //www. youtube. com/watch? v=y. Vr. RJv. Zd. ZHg 18

Image References 19 � 1 A : Centrum. N. p. , n. d. Web.

Image References 19 � 1 A : Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � 2 A : Gill, Victoria. "Could Another Icelandic Volcano Erupt Soon? " BBC News. BBC, 05 Oct. 2010. Web. 04 Nov. 2012. <http: //news. bbc. co. uk/2/hi/8668604. stm>. � 2 B : Google Earth Screen Capture � 3 A: ÓVÁ. "Ingólfur Arnarson. " Flickr. Yahoo!, 17 Feb. 2011. Web. 05 Nov. 2012. <http: //www. flickr. com/photos/2 odinn/5451743423/lightbox/>. � 3 B : "Space Aliens Blamed For Electric Universe. " Space Aliens Blamed For Electric Universe. N. p. , n. d. Web. 04 Nov. 2012. <http: //www. thunderbolts. info/tpod/2007/arch 07/071105 spacealiens. htm>. � 4 A : "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. <http: //pubs. usgs. gov/gip/heimaey/>. � 5 A : Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � 5 B : Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � 6 A : Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � 7 B : "Iceland in Pictures. " Icelandpictures. tumblr. com. N. p. , n. d. Web. 04 Nov. 2012. <http: //icelandpictures. tumblr. com/post/17314265440/vestmannaeyjar>. � 8 A : Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � 9 A : http: //ffden-2. phys. uaf. edu/212_spring 2005. web. dir/philip_fitzgerald/tecniques. htm � 9 B : Volcano. und. nodak. edu. N. p. , n. d. Web. 4 Nov. 2012. <http: //volcano. und. nodak. edu/vwdocs/volc_images/europe_west_asia/heimaey. html>. � 10 A : "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. <http: //pubs. usgs. gov/gip/heimaey/>. � 11 A : "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. <http: //pubs. usgs. gov/gip/heimaey/>. � 12 A : "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. <http: //pubs. usgs. gov/gip/heimaey/>. � 13 A : "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. <http: //pubs. usgs. gov/gip/heimaey/>. � 14 A : http: //drinks. seriouseats. com/images/2011/09/20110901 iceland-500. jpg � 14 B : Col, Ela. Puffin. 2012. Photograph. Heimaey, Iceland. Flickr, 20 June 2012. Web. 4 Dec. 2012. <http: //www. flickr. com/photos/elacol/7427598690/>. � 15 A : Courtesy of Tom Saylor IV, 2012.

Text References � Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey

Text References � Centrum. N. p. , n. d. Web. <http: //www. centrum. is/~edda/heimaey 1. html>. � Einarsson, T. , 1974, The Heimaey eruption in words and pictures: Heimskringla, Reykjavik, 56 p. � "Man Against Volcano: Heimaey, Iceland. " Man Against Volcano: Heimaey, Iceland. N. p. , n. d. Web. 04 Dec. 2012. � Morgan, A. V. "The Eldfell Eruption, Heimaey, Iceland: A 25 -year Retrospective. " Geoscience Canada 27. 1 (2000): 11 -18. Web. 13 Nov. 2012. � <http: //pubs. usgs. gov/gip/heimaey/>. � Simkin, T. , and Siebert, L. , 1994, Volcanoes of the World: Geoscience Press, Tucson, Arizona, 349 p. � Williams, R. S. , and Moore, J. G. , 1983, Man against volcano: The eruption on Heimaey, Vestmannaeyjar, Iceland: U. S. Geological Survey General Interest Publication, 27 p 20