Lake Toba: Difference between revisions
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===The eruption=== |
===The eruption=== |
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:''Main article: [[Toba catastrophe theory]]''. |
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[[Image:Lake_Toba_location.png|thumb|170px|right|Location of Lake Toba shown in red on map.]] |
[[Image:Lake_Toba_location.png|thumb|170px|right|Location of Lake Toba shown in red on map.]] |
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The subsequent collapse formed a [[caldera]] that, after filling with water, created Lake Toba. |
The subsequent collapse formed a [[caldera]] that, after filling with water, created Lake Toba. |
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The eruption lasted perhaps two weeks, but the ensuing "volcanic winter" resulted in a decrease in average global temperatures by 3 to 3.5 degrees Celsius for several years. [[Ice core|Greenland ice core]]s record a pulse of starkly reduced levels of organic carbon sequestration. Very few plants or animals in southeast Asia would have survived, and it is possible that the eruption caused a planet-wide die-off. There is some evidence, based on [[mitochondrial DNA]], that the human race |
The eruption lasted perhaps two weeks, but the ensuing "volcanic winter" resulted in a decrease in average global temperatures by 3 to 3.5 degrees Celsius for several years. [[Ice core|Greenland ice core]]s record a pulse of starkly reduced levels of organic carbon sequestration. Very few plants or animals in southeast Asia would have survived, and it is possible that the eruption caused a planet-wide die-off. There is some evidence, based on [[mitochondrial DNA]], that the human race may have passed through a [[genetic bottleneck]] within this timeframe, reducing genetic diversity below what would be expected from the age of the species. According to the [[Toba catastrophe theory]] proposed by Stanley H. Ambrose of the [[University of Illinois at Urbana-Champaign]] in 1998, human populations may have been reduced to only a few tens of thousands of individuals by the Toba eruption. |
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=== More recent activity=== |
=== More recent activity=== |
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Revision as of 07:35, 6 October 2006
| Lake Toba | |
|---|---|
| Coordinates | 2°37′N 98°49′E / 2.617°N 98.817°E |
| Basin countries | North Sumatra, Indonesia |
| Max. length | 100 km |
| Max. width | 30 km |
| Surface area | 1130 km² |
| Max. depth | 529 m |
| Water volume | 240 km³ |
| Surface elevation | 905 m |
Lake Toba (Indonesian: Danau Toba) is a large lake, 100 km long and 30 km wide, in the middle of the northern part of the Indonesian island of Sumatra with a surface elevation of about 900 m (3000 feet), stretching from 2°53′N 98°31′E / 2.88°N 98.52°E to 2°21′N 99°06′E / 2.35°N 99.1°E.
Geology
In 1949 the Dutch geologist Rein van Bemmelen reported that Lake Toba was surrounded by a layer of ignimbrite rocks, and that it was a large volcanic caldera. Later researchers found rhyolite ash similar to that in the ignimbrite around Toba (now called Young Toba Tuff to distinguish it from layers deposited in previous explosions) in Malaysia and India, 3000 km away. Oceanographers discovered Toba ash, with its characteristic chemical "fingerprint", on the floor of the eastern Indian Ocean and the Bay of Bengal.
The eruption
The Toba eruption (the Toba event) occurred at what is now Lake Toba about 71,500 ± 4000 years ago. It had an estimated Volcanic Explosivity Index of 8, making it the most recent supervolcano eruption and probably the largest volcanic eruption within the last two million years. Bill Rose and Craig Chesner of Michigan Technological University deduced that the total amount of erupted material was about 2800 cubic km (670 cubic miles) — around 2000 km³ of ignimbrite that flowed over the ground and around 800 km³ that fell as ash, with the wind blowing most of it to the west. By contrast, the 1980 eruption of Mount St. Helens ejected around 1 cubic km of material, whilst the largest volcanic eruption in historic times, at Mount Tambora in 1815, emitted the equivalent of around 100 cubic kilometres of dense rock and created the "Year Without a Summer" as far away as North America.
The Toba eruption was the last of a series of at least three caldera-forming eruptions which have occurred at the volcano. Earlier calderas were formed around 700,000 and 840,000 years ago[1].
To give an idea of its magnitude, consider that although the eruption took place in Indonesia, it deposited an ash layer approximately 15 cm (6 in) thick over the entire Indian subcontinent; at one site in central India, the Toba ash layer today is up to 6 m (20 feet) thick[citation needed].
The subsequent collapse formed a caldera that, after filling with water, created Lake Toba.
The eruption lasted perhaps two weeks, but the ensuing "volcanic winter" resulted in a decrease in average global temperatures by 3 to 3.5 degrees Celsius for several years. Greenland ice cores record a pulse of starkly reduced levels of organic carbon sequestration. Very few plants or animals in southeast Asia would have survived, and it is possible that the eruption caused a planet-wide die-off. There is some evidence, based on mitochondrial DNA, that the human race may have passed through a genetic bottleneck within this timeframe, reducing genetic diversity below what would be expected from the age of the species. According to the Toba catastrophe theory proposed by Stanley H. Ambrose of the University of Illinois at Urbana-Champaign in 1998, human populations may have been reduced to only a few tens of thousands of individuals by the Toba eruption.
More recent activity
Smaller eruptions have occurred at Toba since. The small cone of Pusukbukit has formed on the southwestern margin of the caldera and lava domes. The most recent eruption may have been at Tandukbenua on the northwestern caldera edge, since the present lack of vegetation could be due to an eruption within the last few hundred years [2].
Some parts of the caldera have experienced uplift due to partial refilling of the magma chamber, for example pushing Samosir Island and the Uluan Peninsula above the surface of the lake. The lake sediments on Samosir Island show that it has been uplifted by at least 450 metres [3] since the cataclysmic eruption. Such uplifts are common in very large calderas, apparently due to the upward pressure of unerupted magma. Toba is probably the largest resurgent caldera on Earth. Large earthquakes have occurred in the vicinity of the volcano more recently, notably in 1987 along the southern shore of the lake at a depth of 11 km[4]. Other earthquakes have occurred in the area in 1892, 1916, and 1920-1922[5].
Lake Toba lies near a fault line which runs along the centre of Sumatra called the Sumatra Fracture Zone [6]. The volcanoes of Sumatra and Java are part of the Sunda Arc, a result of the northeasterly movement of the Indo-Australian Plate which is sliding under the eastward-moving Eurasian Plate. The subduction zone in this area is very active: the seabed near the west coast of Sumatra has had several major earthquakes since 1995, including the 9.3 2004 Indian Ocean Earthquake and the 8.7 2005 Sumatra earthquake, the epicenters of which were around 300 km from Toba.
People
Most of the people who live around Lake Toba are ethnically Bataks. Traditional Batak houses are noted for their distinctive roofs (which curve upwards at each end, as a boat's hull does) and their colorful decor.
See also
Notes
- ^ http://volcano.und.nodak.edu/vwdocs/volc_images/southeast_asia/indonesia/toba.html
- ^ http://www.volcanodiscovery.com/volcano-tours/volcanoes/indonesia/sumatra/toba/
- ^ http://volcano.und.nodak.edu/vwdocs/volc_images/southeast_asia/indonesia/toba.html
- ^ http://earthquake.usgs.gov/eqcenter/eqarchives/significant/sig_1987.php
- ^ http://volcano.und.nodak.edu/vwdocs/volc_images/southeast_asia/indonesia/toba.html
- ^ http://volcano.und.nodak.edu/vwdocs/volc_images/southeast_asia/indonesia/toba.html
References
- Rampino, Michael R. and Stephen Self (1993). "Climate-volcanism feedback and the Toba eruption of 74,000 Years Ago". Quaternary Research. 40 (3): 269–280.
- Vazquez, Jorge A. and Mary R. Reid (2004). "Probing the accumulation history of the voluminous Toba Magma". Science. 305 (5686): 991–994.
