Zavaritski Caldera
Template:Short description Template:Use dmy dates Template:Use British English Template:Infobox mountain
Template:Langr Caldera (Template:Langx, Template:Transliteration), also spelled "Template:Langr" and "Template:Langr", is a caldera system located in the centre of Simushir island, in the central Kuril Islands, Russia. The volcano is named after Template:Langr, a scientist of the Academy of Sciences of the Soviet Union.
Geology
The Zavaritski volcano contains three nested calderas, measuring Template:Convert, Template:Cvt and Template:Cvt in diameter. The youngest caldera, which is partially filled by Lake Template:Langr, was formed during the Holocene and features several young volcanic cones and lava domes. The lake surface sits at an elevation of Template:Convert above sea level, with the lake bottom at Template:Val below sea level. Lake sediments overlying pumice deposits indicate that a previous caldera lake surface existed Template:Cvt above sea level.
The last reported explosive eruption was recorded in November 1957. This destroyed a Template:Cvt diameter cone[1] that reportedly grew pre-eruption and had formed a peninsula extending into the lake from the northeast caldera wall. The eruption filled the northwest section of the lake, including the emplacement of a Template:Cvt wide, Template:Cvt high dome.
1831 eruption
Research indicates that Template:Langr Caldera may have been the source of a high-magnitude explosive eruption that occurred in 1831, during the Northern Hemisphere summer.[2]
Evidence for the eruption includes sulfate peaks in polar ice cores and from historical observations of atmospheric phenomena in Japanese records (such as observations of an abnormally colored sun). It is thought that the mass injection of sulfur from the eruption caused Northern Hemisphere climate cooling of Template:Convert, coincided with fluctuations in the Indian and African monsoons, and preceded major famines (including the [[Guntur famine of 1832|Template:Langr famine of 1832]] in India). However, the source of this major eruption has remained a mystery.
The researchers, led by volcanologist William Hutchison, conducted geochemical analyses of several Greenland ice cores. They found, coinciding with the sulphate peaks from the 1831 eruption, microscopic layers of tephra that chemically matched deposits from the most recent Plinian Template:Langr eruption, dated to the early 19th century. Modelling suggests that the eruption could have been a VEI 5/6-magnitude eruption event. The reconstructed radiative forcing of the eruption is comparable to the 1991 eruption of Mount Pinatubo, and may account for the climatic cooling observed between 1831–1833.
See also
References
External links
- Template:Cite gvp
- Aerial image retrieve from NASA Technical Reports Server on 19 April 2007.