Santa María (volcano): Difference between revisions
Chris.urs-o (talk | contribs) |
No edit summary |
||
| Line 5: | Line 5: | ||
| Elevation = 3,772 metres (12,372 ft) |
| Elevation = 3,772 metres (12,372 ft) |
||
| Location = [[Quetzaltenango Department]], [[Guatemala]] |
| Location = [[Quetzaltenango Department]], [[Guatemala]] |
||
| Range = [[Sierra Madre de Chiapas|Sierra Madre]] |
| Range = fjgfjljgalkj;alallk[[Sierra Madre de Chiapas|Sierra Madre]] |
||
| Prominence = |
| Prominence = |
||
| Coordinates = {{coord|14.756|N|91.552|W|type:mountain}} |
| Coordinates = {{coord|14.756|N|91.552|W|type:mountain}} |
||
| Topographic map = |
| Topographic map = |
||
| Type = [[Stratovolcano]] |
| Type = [[Stratovolcano]] |
||
| Age = |
| Age = 344354354 |
||
| Last eruption= 2009 (continuing) |
| Last eruption= 2009 (continuing) |
||
| First ascent = |
| First ascent = |
||
Revision as of 16:58, 2 February 2010
| Santa María | |
|---|---|
 |
Santa María Volcano is a large active volcano in the Western Highlands of Guatemala, close to the city of Quetzaltenango. Prior to the Spanish Conquest it was called Gagxanul in the local K'iche' language.[1] Its eruption in 1902 was one of the four largest eruptions of the 20th century, after the 1912 Novarupta and 1991-1994 Pinatubo eruptions. It was also the third large (VEI 4+) eruption of that one year, after Mount Pelée in Martinique (VEI 4)[2] and Soufrière in St. Vincent(VEI 4)[3]. It is one of the five biggest eruptions of the past 200 (and probably 300) years.[4]
Geological history
Santa María is of the Sierra Madre range of volcanoes, which extends along the western edge of Guatemala, separated from the Pacific Ocean by a broad plain. The volcanoes are formed by the subduction of the Cocos Plate under the Caribbean Plate.
Eruptions at Santa María are estimated to have begun about 30,000 years ago. For several thousand years, eruptions seem to have been small and frequent, building up the large cone of the volcano, reaching about 1,400 metres (4,600 ft) above the plain on which the nearby city of Quetzaltenango sits. Following the cone-building eruptions, activity seems to have changed to a pattern of long periods of repose followed by the emission of small lava flows from vents on the flanks.
The cone built by the eruptions had a volume of about 10 cubic kilometres (2.4 cu mi), and consisted of a mixture of basalt and andesite lavas.
1902 eruption
The first eruption of Santa Maria in the recorded history occurred in October 1902. Before 1902 the volcano had been dormant for at least 500 years and possibly several thousand years, but its awakening was clearly indicated by a seismic swarm in the region starting in January 1902. The eruption began on 24 October, and the largest explosions occurred over the following two days, ejecting an estimated 5.5 cubic kilometres (1.3 cu mi) of magma. The eruption was one of the largest of the 20th century, only slightly less in magnitude to that of Mount Pinatubo in 1991. The eruption had a VEI of 6, thus being 'Colossal'. [5]
The pumice formed in the climactic eruption fell over an area of about 273,000 square kilometres (105,000 sq mi), and volcanic ash was detected as far away as San Francisco, 4,000 kilometres (2,500 mi) away. The eruption tore away much of the south-western flank of the volcano, leaving a crater about 1 kilometre (0.6 mi) in diameter and about 300 metres (980 ft) deep, stretching from just below the summit to an elevation of about 2,300 metres (7,500 ft).
Because of the lack[6] of previous Holocene activity at Santa María, local people did not recognise the preceding seismicity as warning signs of an eruption. At least 5,000 people died as a result of the eruption itself, and a subsequent outbreak of malaria killed many more.
Santiaguito
The 1902 eruption was followed by 20 years of dormancy. In 1922, new eruptions began, with the extrusion of a lava dome in the crater left by the 1902 eruption. The lava dome was dacitic in composition[7] . The dome was christened Santiaguito, and since then, activity has been virtually constant. Santiaguito now reaches a height of about 2,500 metres (8,200 ft), and has a volume of about 1 cubic kilometre (0.24 cu mi). From the summit of Santa María, it is possible to look down on the eruptions at Santiaguito a mile below.
Dome growth at Santiaguito has alternated between growth caused by the emission of lava flows, and inflation caused by the injection of magma into the middle of the dome. These dome growth types are described by volcanologists as exogenous and endogenous respectively. Activity has been concentrated at several different vents, and Santiaguito now has the appearance of several overlapping domes. The currently active vent is El Caliente. [8] There are three other domes - El Brujo, El Mitad and El Monje.[9]
Although most of Santiaguito's eruptive activity has been relatively gentle, occasional larger explosions have occurred. In 1929, part of the dome collapsed, generating pyroclastic flows which killed anywhere from several hundred up to 5,000 people. Occasional rockfalls have generated smaller pyroclastic flows, and vertical eruptions of ash to heights of a few kilometres above the dome are common.
Volcanic hazards at Santa María
The areas to the south of Santa María are considerably affected by volcanic activity at Santiaguito. Currently, the most common volcanic hazard at Santa María is lahars, which frequently occur in the rainy season due to heavy rainfall on loose volcanic deposits. The town of El Palmar, 10 kilometres (6 mi) from Santiaguito, has been destroyed twice by lahars from Santiaguito, and infrastructure such as roads and bridges have been repeatedly damaged. Lahar deposits from Santiaguito have affected rivers all the way downstream to the Pacific Ocean.
Lava flows do not occur frequently from Santiaguito, and tend not to stretch more than a few kilometres from the dome. The magma at Santiaguito is rich in silica and is thus highly viscous. Flows are therefore very slow-moving and are of little danger to human life, although property damage may occur. Fast-moving pyroclastic flows can occur, and these may travel several kilometres from the dome.
One hazard which could be devastating is the collapse of Santa María itself. The 1902 crater has left the southern flank of the mountain above Santiaguito highly over-steepened, and a large earthquake or eruption from Santiaguito could trigger a huge landslide, which might cover up to 100 square kilometres (39 sq mi). However, this is thought to be unlikely in the short term.
In light of the threat it poses to nearby populations, Santa María has been designated a Decade Volcano, identifying it as a target for particular study by volcanologists to mitigate any future natural disasters at the volcano.
See also
- List of volcanoes in Guatemala
- List of volcanic eruptions by death toll
- Timetable of major worldwide volcanic eruptions
References
- Notes
- ^ Recinos 1952, 1986, p.69.
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1600-12=&volpage=erupt
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1600-15=&volpage=erupt
- ^ "Large Holocene Eruptions". Global Volcanism Program. Smithsonian Institution. Retrieved 12 October 2008.
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03=&volpage=erupt
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03=&volpage=erupt
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03=
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03=
- ^ http://www.volcano.si.edu/world/volcano.cfm?vnum=1402-03=&volpage=synsub
- Bibliography
- Bunzendahl, E.; Bluth, G. J.; Rose, W. I.; Reif, S. L.; Matias, O. (2001), Developing a Long-term Hazard Mitigation Plan for Consequent Volcanic Sedimentation Hazards at Santiaguito Dome Complex, Guatemala, American Geophysical Union, Fall Meeting 2001, abstract #V41A-0974
- Harris, A. J.; Flynn, L. P.; Rose, W. I.; Matias, O.; Cornejo, J. (2002), The extrusion of lava dome and block lava flow units at Santiaguito, 1922-2002, American Geophysical Union, Fall Meeting 2002, abstract #V12A-1399
- Recinos, Adrian (1986). Pedro de Alvarado: Conquistador de México y Guatemala (2nd ed.). Guatemala: CENALTEX Centro Nacional de Libros de Texto y Material Didáctico "José de Pineda Ibarra". OCLC 243309954.
{{cite book}}: templatestyles stripmarker in|author=at position 1 (help)CS1 maint: numeric names: authors list (link) Template:Es icon