Weekly Ocean News

WEEK TWO: 6-10 February 2017


Items of Interest

Ocean in the News


REPORTS FROM THE FIELD --

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Concept of the Week: The Birth of Surtsey, A Volcanic Island

In early November 1963, cod fishers plying the waters of the North Atlantic south of Iceland observed what appeared to be smoke or steam emanating from the distant ocean surface. They were witnessing the beginnings of a volcanic eruption that ultimately would give birth to a new island later named Surtsey after Surtur, the fire giant of Norse mythology. Surtsey is located at 63.4 degrees N, 20.3 degrees W or 33 km (20 mi) south of the coast of Iceland. Volcanic activity was nothing new to the fishers who lived on the nearby volcanic Westman Islands (Vestmannaeyjar). These islands as well as the main island of Iceland straddle the Mid-Atlantic Ridge, a divergent tectonic plate boundary where hot molten lava wells up from the Earth's mantle, cools and solidifies into new oceanic crust.

Eruptions that produced Surtsey began on the ocean floor, some 130 m (427 ft) below sea level. The accumulating lava, cinders, and ash first emerged from the sea on 15 November 1963. Over the next 3.5 years, episodic eruptions built an island that eventually covered 2.5 square km (1 square mi) and attained a maximum elevation of 171 m (560 ft) above sea level. The initial eruptions were explosive as hot magma interacted with cold seawater producing dark jets of ash and steam that shot up to 200 m (656 ft) above two main volcanic vents. At this time, clouds of ash and steam rose into the atmosphere to altitudes perhaps as great as 10 km (6.2 mi). Subsequent eruptions were much more peaceful, consisting of quiescent flows of lava. When the eruptions ceased in early June 1967, a cubic kilometer of ash and lava had built up on the ocean floor with 9% of this volcanic material above sea level.

No volcanic activity has occurred on Surtsey since 1967 and geologists consider the volcanic island to be extinct with little risk of future eruptions. Nonetheless, Surtsey remains off limits to visitors except for scientists who obtain permission from the Icelandic government. The island offers scientists a unique opportunity to study not only the geology but also the establishment of plants and animals on the island, a process known as ecological succession. For example, by 1987, some 25 species of higher plants were growing on the initially barren island and 20 species of birds were nesting there.

Unless volcanic activity begins anew, the future is not bright for Surtsey. Some geologists predict that in a hundred years or so the island will be reduced to scattered stacks of rock. The island is composed of basaltic rock that is particularly vulnerable to weathering and erosion, ocean waves are eroding its shores, and the island is gradually sinking into the sea. Scientists reported a total subsidence of about 1.1 m (3.6 ft) between 1967 and 1991. Compaction of the volcanic material and the underlying sea-floor sediments are likely causes of the subsidence. For NASA topographical images of Surtsey, go to http://denali.gsfc.nasa.gov/research/garvin/surtsey.html . These images were obtained using a scanning airborne laser altimeter.

Concept of the Week: Questions
  1. The volcanism responsible for the formation of Surtsey was associated with a [(divergent)(convergent)] tectonic plate boundary.
  2. At present on Surtsey, erosive forces [(are)(are not)] prevailing over volcanic activity.

Historical Events


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Prepared by DS Ocean Central Staff and Edward J. Hopkins, Ph.D.,
email
hopkins@aos.wisc.edu
© Copyright, 2017, The American Meteorological Society.