- Rincón de la Vieja Volcano
Infobox Mountain
Name = Rincón de la Vieja
Photo = Rincon de la Vieja.jpg
Caption = Rincón de la Vieja
Elevation = convert|1916|m|ft|0|lk=off
Location =Costa Rica
Range =Cordillera de Guanacaste
Coordinates = coord|10|50|N|85|19|W|type:mountain
Type =Complex volcano
Last eruption =1998 Rincón de la Vieja is an active andesitic
complex volcano in north-westernCosta Rica , about 25 km from Liberia, in the province of Guanacaste. Its name means "The Old Woman's Corner", a reference to a local legend about a girl whose lover was thrown into the crater by her father; she became a recluse living on the mountain, and was credited with powers of healing.Rincón de la Vieja stands 1916
metre s abovesea level , and its summit is the highest point inRincón de la Vieja Volcano National Park . It erupted most recently in February 1998. The volcano has a large number offumarole s andhot springs on its slopes.Rincón de la Vieja is one of seven active Costa Rican volcanoes: the others are Poás, Irazú, Miravalles, Orosí, Arenal, and Turrialba.
Geology
Rincón de la Vieja is a ridge-shaped massif, with several volcanic vents lying along a northwest-southeast axis. Several craters and peaks exist, with Santa María peak being the highest at 1916m above sea level. Von Seebach peak, 1895m above sea level, has been the site of most historical eruptions.
Little is known about Rincón de la Vieja's early eruptive history. It lies within a larger
caldera , which indicates that a very large eruption probably occurred thousands of years ago. Analysis of nearbypyroclastic flow deposits shows that they were erupted in a moderately large eruption about 3500 years ago, and the first recorded eruption of the volcano took place in1765 .Since then, many minor eruptions have occurred, the most recent in 1998. They have mostly occurred at a crater near Von Seebach peak, and have been characterised by
strombolian and vulcanian activity in which eruptions are confined to the crater, and ash is erupted to moderate heights. The active crater is currently filled with a hot, acidiccrater lake VNUM | 1=1405-02= | 2=Rincón de la Vieja] .Geothermal energy
Large number of hot pools and areas of bubbling mud are found in two areas on the slopes of the volcano, indicating substantial reserves of
geothermal energy . Investigations have been carried out into the feasibility of tapping these reserves, and the volcano is estimated to have a generating potential of 140megawatt s. However, as the area is protected within anational park , drilling has so far been limited to test wells. Further drilling will require approval after studies of the likely environmental impact. [Huttrer G.W. (2001), "The status of world geothermal power generation 1995-2000", Geothermics, v.30, p.1-27]Tourism
Hikers may climb to the crater and guides experienced in wildlife, birdwatching, geology and other interests are available. Several lodges, resorts and hotels in the area offer hiking, forest canopy tours, horseback riding, river-rafting, all-terrain-vehicle riding and wall-climbing. The area is cooler than the Guanacaste beaches.
ee also
*
List of volcanoes in Costa Rica References
External links
* [http://www.ovsicori.una.ac.cr/vulcanologia/volcanes/rincon_vieja.htm Costa Rican Vulcanologic and Seismologic Observatory: Rincón de la Vieja]
* [http://volcano.und.nodak.edu/vwdocs/current_volcs/costa_rica/rincon.html Rincón de la Vieja, Costa Rica - descriptions and pictures of volcanic activity]
* [http://www.wikicostarica.com:16080/index.php/Rincon_de_la_Vieja_National_Park Videos and photos of Rincon de la Vieja]
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