Iceland hotspot
The Iceland hotspot is a hotspot which is partly responsible for the high volcanic activity which has formed the island of Iceland.
Evidence
Iceland is one of the most active volcanic regions in the world, with eruptions occurring on average roughly every five years. About a third of the basaltic lavas erupted in recorded history have been produced by Icelandic eruptions. Notable eruptions have included that of Laki in 1783, which was the largest basaltic eruption ever witnessed, and several eruptions beneath ice caps, which have generated devastating glacial bursts, most recently in 1996.
Iceland's location astride the Mid-Atlantic Ridge, where the Eurasian and North American Plates are moving apart, is partly responsible for this intense volcanic activity, but an additional cause is necessary to explain why Iceland is a substantial island while the rest of the ridge mostly consists of seamounts, with peaks below sea level. It is believed that a hotspot must lie beneath the island, enhancing the volcanism already caused by plate separation.
As well as driving volcanism in the centre of the island, the hotspot is also believed to feed magma to the Reykjanes ridge, another region of elevated volcanism to the southwest of Iceland's main volcanic zone.
Nature of the hotspot
Iceland's hotspot is believed to be quite narrow, perhaps 100 km across, and extends down to at least 400–650 km beneath the Earth's surface, and possibly down to the core-mantle boundary. As well as being a region of higher temperature than the surrounding mantle, it is also believed to have a higher concentration of water. The presence of water in magma reduces the melting temperature, and so the wetness of the Iceland hotspot probably also plays a role in enhancing Icelandic volcanism.
Some geologists have questioned whether the Iceland hotspot has the same origin as other hotspots such as the Hawaii hotspot. While the Hawaiian island chain and the Emperor Seamounts show a clear time-progressive volcanic track caused by the movement of the Pacific Plate over the Hawaiian hotspot, no such track can be seen at Iceland, possibly because the plume which is assumed to cause it may have been located beneath the thick Greenland craton for a significant time.
Studies suggest that the hotspot is only 50-100 K hotter than its surroundings, which may not be a great enough difference to drive a buoyant plume. There is an ongoing discussion whether the hotspot is caused by a deep mantle plume or originates at a much shallower depth.
See also
References
- Allen, RM; Nolet, G; Morgan, WJ; et al. (1999). "The thin hot plume beneath Iceland." Geophysical Journal International. 137, 51-63.
- Foulger, GR; Anderson, DL (2005). "A cool model for the Iceland hotspot." Journal of Volcanology and Geothermal Research. 141, 1-22.
- Nichols, ARL; Carroll, MR; Höskuldsson, Á (2002). "Is the Iceland hot spot also wet? Evidence from the water contents of undegassed submarine and subglacial pillow basalts." Earth and Planetary Science Letters. 202, 77-87.