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Soufrière Hills

Ash fall from Soufrière Hills volcano
Elevation 915 metres (3,002 feet)[1]
Prominence 915 m (3,002 ft)[1]
Location
Location Montserrat, Caribbean
Coordinates 16°43′N 62°11′W / 16.717°N 62.183°W / 16.717; -62.183
Geology
Type Stratovolcano
Last eruption February 11, 2010
2009 ash and steam plume, Soufriere Hills Volcano. Gray deposits that include pyroclastic flows and volcanic mudflows (lahars) are visible extending from the volcano toward the coastline. NASA ISS photo, October 11, 2009. See File:Ash and Steam Plume, Soufriere Hills Volcano, Montserrat.jpg for a higher-resolution version of this photo.
Soufrière Hills before and after a recent partial dome collapse.

The Soufrière Hills volcano (French "Sulphur" Hills) is an active complex stratovolcano with many lava domes forming its summit on the Caribbean island of Montserrat. After a long period of dormancy, it became active in 1995, and has continued to erupt ever since. Its eruptions have rendered more than half of Montserrat uninhabitable, destroying the capital city, Plymouth, and causing widespread evacuations: about two thirds of the population left the island. Seismic activity had occurred in 1897–1898, 1933–1937, and again in 1966–1967, but the eruption that began on July 18, 1995, was the first since the 17th century.[2] When pyroclastic flows and mudflows began occurring regularly, Plymouth was evacuated, and a few weeks later a pyroclastic flow covered the city in several metres of debris. A large eruption on June 25, 1997, resulted in the deaths of nineteen people. The island's airport was directly in the path of the main pyroclastic flow and was completely destroyed.[3] Montserrat's tourist industry was also destroyed. However, it is now regenerating. The governments of the United Kingdom and Montserrat led the aid effort, including a £41 million package provided to the people of Montserrat; however, riots followed as the people protested that the British Government was not doing enough to aid relief.[4]

The volcano is andesitic in nature and the current pattern of activity includes periods of dome growth, punctuated by brief episodes of dome collapse which result in pyroclastic flows, ash venting, and explosive eruption. On December 24, 2006, streaks of red from the pyroclastic flows became visible. On January 8, 2007, an evacuation order was issued for areas in the Lower Belham Valley, affecting an additional 100 people.

The most devastating eruption was at Soufriere Hills Volcano starting at 11:27 pm local time on Monday, 28 July 2008, without any precursory activity. Pyroclastic flow lobes reached Plymouth. These involved juvenile material originating in the collapse of the eruption column. Further, a small part of the eastern side of the lava dome collapsed, generating a pyroclastic flow in Tar River Valley. Several large explosions were registered, with the largest at approximately 11:38 pm. The height of the ash column was estimated at 12 kilometres (40,000 feet) above sea level.

The volcano has become one of the most closely monitored volcanoes in the world since its eruption began, with the Montserrat Volcano Observatory ([1]) taking detailed measurements and reporting on its activity to the government and population of Montserrat. The observatory is operated by the British Geological Survey under contract to the government of Montserrat.

Results: in the October 9, 2008, issue of the journal Science suggest that two interconnected magma chambers lie beneath the surface of the volcano on Montserrat – one six kilometers below the surface and the other at 12 kilometers below the surface. They also show a link between surface behavior and the size of the deeper magma chamber.[5][6]

On 5 February 2010, a vulcanian explosion simultaneously propelled pyroclastic flows down several sides of the mountain, and on 11 February 2010, a partial collapse of the lava dome sent large ash clouds over sections of several nearby islands including Guadeloupe and Antigua. Inhabited areas of Montserrat itself received very little ash accumulation through either event. [7] Soufrière Hills is the namesake of the Jimmy Buffett song "Volcano".[8]


Contents

Gallery

See also

References

  1. ^ a b This elevation is for Chance's Peak, the traditional high point. However the lava dome in English's Crater is currently estimated at over 930 m (2006): see The CIA World Factbook on Montserrat.
  2. ^ "Soufrière Hills". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1600-05=. 
  3. ^ "BBC country profile: Montserrat". September 22, 2009. http://news.bbc.co.uk/1/hi/world/americas/country_profiles/3666502.stm. Retrieved 2008-03-08. 
  4. ^ UK citizenship for island outposts | The Guardian | Guardian Unlimited
  5. ^ "Implications of Magma Transfer Between Multiple Reservoirs on Eruption Cycling.". Science 322 (5899): 246–248. October 2008. doi:10.1126/science.1161297. http://www.sciencemag.org/cgi/content/abstract/322/5899/246. Retrieved 2008-10-09. 
  6. ^ Multiple Magma Reservoirs Affect Volcanic Eruption Cycles Newswise, Retrieved on October 9, 2008.
  7. ^ [http://www.montserratvolcanoobservatory.info/index.php?option=com_content&view=section&layout=blog&id=9&Itemid=94&lang=en Montserrat Volcano Observatory]
  8. ^ Jimmy Buffett "Live in Anguilla" CD/DVD.

External links








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