Jump to content

Shield volcano

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Zorrobot (talk | contribs) at 14:47, 26 July 2008 (robot Adding: sv:Sköldvulkan). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Shield volcano

A shield volcano is a large volcano with shallow-sloping sides. The name derives from a translation of "Skjaldbreiður", an Icelandic shield volcano whose name means "broad shield," from its resemblance to a warrior's shield.

Information

Shield volcanoes are formed by lava flows of low viscosity — lava that flows easily. Consequently, a volcanic mountain having a broad profile is built up over time by flow after flow of relatively fluid basaltic lava issuing from vents or fissures on the surface of the volcano. Many of the largest volcanoes on Earth are shield volcanoes. The largest in terms of area covered is Mauna Loa of Hawaii; the tallest measured from its base under the ocean, however, is Mauna Kea of Hawaii. All the volcanoes in the Hawaiian Islands are shield volcanoes.

Geographical extent

Shield volcanoes can be so large that they are sometimes considered to be a mountain range, such as the Ilgachuz Range and the Rainbow Range, both of which are located in Canada. These shield volcanoes formed when the North American Plate moved over a hotspot similar to the one feeding the Hawaiian Islands, called the Anahim hotspot. Shield volcanoes can be found in many places around the world, including Australia, Ethiopia, and the Galapagos Islands. The Piton de la Fournaise, on Reunion Island, is one of the most active shield volcanoes on earth, with one eruption per year on average.

Magma

The viscosity of magma as it approaches the surface is dependent on its temperature and composition. Shield volcanoes in the Hawaiian Islands erupt magma as hot as 1,200 °C (2,200 °F), compared with 850 °C (1,560 °F) for most continental volcanoes, which are usually composed of acidic lava. Because of the fluidity of the lava, major explosive eruptions do not occur. The most severe explosions occur if water enters a vent, although expanding gases in the magma can produce spectacular fountaining of the low viscosity lava.

Solar system occourances

Mauna Kea, a shield volcano, on the Island of Hawaii with a light dusting of snow.

Shield volcanoes are known to form on other planets

  • The largest known mountain in the solar system, Olympus Mons on Mars, is a shield volcano thought to be dormant.
  • Shield volcanoes on Mars are higher and much more massive than those on Earth, likely due to lack of tectonic plates on Mars.

On Earth, because of plate tectonics, hotspot volcanoes eventually move away from the source of their magma and the volcanoes are individually less massive than might otherwise be the case. Shield volcanoes usually occur along constructive boundaries or above hotspots. However, the numerous large shield volcanoes of the Cascades of northern California and Oregon are over a more complex environment.

For more information on volcanoes go to Strato volcano or cinder cone volcano

Examples

Skjaldbreiður, eponymous for a shield volcano
Dark profile of Hualālai, showing typical shape of a shield volcano
Mount Edziza, a massive shield volcano in northwestern British Columbia, Canada

References

Retrieved from "https://en.wikipedia.org/w/index.php?title=Shield_volcano&oldid=228016446"