Difference between revisions of "Volcano"

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[[Image:Volcano.jpg|thumb|300px|Snow-covered Kanaga Volcano in Alaska erupts a small column of tephra, gas, and steam. Kanaga is a stratovolcano. View is toward the west.]]A '''volcano''' is a vent of some kind in the earth's crust through which [[magma]] is ejected.  The magma frequently builds up in layers, resulting in the formation of mountains.  Different types of magma produce different kinds of structures.  Hot basaltic [[lava]], which has low viscosity, tends to produce flat shield volcanoes because it can flow long distances before cooling.  [[Andesite]] and [[dacite]] lava generally produce cones, like those seen in the cases of [[Mt. Fuji]] and [[Mt. Rainier]], because the higher viscosity lava flows build up more dramatically near the vent
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[[Image:Volcano.jpg|thumb|300px|Snow-covered Kanaga Volcano in Alaska erupts a small column of tephra, gas, and steam. Kanaga is a stratovolcano. View is toward the west.]]
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A ''volcano'' forms when [[magma]], in the form of [[lava]], is able to breach the surface of the [[Earth]]. Many volcanoes tend to resemble [[mountains]], although some are so large that they form entire [[Island|islands]], as is the case of [[Mauna Loa]]. Volcanoes come in three main types, stratovolcano (also composite cone), shiled volcano, and cinder cone.
  
 
[[Category:Volcanology]]
 
[[Category:Volcanology]]

Revision as of 04:02, December 15, 2007

Snow-covered Kanaga Volcano in Alaska erupts a small column of tephra, gas, and steam. Kanaga is a stratovolcano. View is toward the west.

A volcano forms when magma, in the form of lava, is able to breach the surface of the Earth. Many volcanoes tend to resemble mountains, although some are so large that they form entire islands, as is the case of Mauna Loa. Volcanoes come in three main types, stratovolcano (also composite cone), shiled volcano, and cinder cone.