Fumarole

"Solfatara" redirects here. For the volcanic crater in Italy, see Solfatara (volcano).
Fumaroles on Mount Redoubt in Alaska
A fumarole at Halema`uma`u crater
Fumarole at Námafjall, Iceland
Sampling gases at a fumarole on Mount Baker in Washington, United States
Fumaroles at Vulcano, Sicily

A fumarole (ultimately from the Latin fumus," smoke") is an opening in a planet's crust, often in the neighborhood of volcanoes, which emits steam and gases such as carbon dioxide, sulfur dioxide, hydrogen chloride, and hydrogen sulfide. The steam forms when superheated water vaporizes as its pressure drops when it emerges from the ground. The name solfatara, from the Italian solfo, sulfur (via the Sicilian language, compare Solfatara (volcano)), is given to fumaroles that emit sulfurous gases.

Fumaroles may occur along tiny cracks or long fissures, in chaotic clusters or fields, and on the surfaces of lava flows and thick deposits of pyroclastic flows. A fumarole field is an area of thermal springs and gas vents where magma or hot igneous rocks at shallow depth release gases or interact with groundwater.[1] From the perspective of groundwater, fumaroles could be described as a hot spring that boils off all its water before the water reaches the surface.

Fumaroles may persist for decades or centuries if located above a persistent heat source; or they may disappear within weeks to months if they occur atop a fresh volcanic deposit that quickly cools. The Valley of Ten Thousand Smokes, for example, was formed during the 1912 eruption of Novarupta in Alaska. Initially, thousands of fumaroles occurred in the cooling ash from the eruption, but over time most of them have become extinct.

There are an estimated four thousand fumaroles within the boundaries of Yellowstone National Park in the United States of America. In April 2006 a fumarole killed three ski-patrol workers east of Chair 3 at Mammoth Mountain Ski Area in California. The workers were overpowered by toxic fumes (a mazuku) that had accumulated in a crevasse they had fallen into.[2] Another example is an array of fumaroles in the Valley of Desolation in Morne Trois Pitons National Park in Dominica.

Fumaroles emitting sulfurous vapors form surface deposits of sulfur-rich minerals; places in which these deposits have been mined include:

On Mars

The formation called Home Plate at Gusev Crater on Mars which was examined by the Mars Exploration Rover (MER) Spirit is suspected to be the eroded remains of an ancient and extinct fumarole.[4]

See also

References

  1. ↑ Compare: Neuendorf, Klaus K. E. (2005). Jackson, Julia A.; Mehl, James P.; Neuendorf, Klaus K. E., eds. Glossary of Geology. Springer Science & Business Media. p. 257. ISBN 9780922152766. Retrieved 2015-06-06. fumarole field[:] A group of cool fumaroles.
  2. ↑ Hymon, Steve; Covarrubias, Amanda (2006-04-09). "How Routine Turned to Tragedy at Mammoth". Los Angeles Times. Retrieved 2011-05-09.
  3. ↑ Global Volcanism Program, National Museum of Natural History, Smithsonian Institution
  4. ↑ R.V.Morris, S.W.Squyres, et al. "The Hydrothermal System at Home Plate in Gusev Crater, Mars". Lunar & Planetary Science XXXIX(2008)

External links

Wikimedia Commons has media related to Fumaroles.
This article is issued from Wikipedia - version of the Saturday, January 02, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.