nannoh
- 202
- 0
Here is some information about the Toba Event mentioned earlier by Bystander
Volcanic winter and accelerated glaciation following the Toba super-eruption
From
http://www.nature.com/nature/journal/v359/n6390/abs/359050a0.html
Sort of makes human influences on "global warming" or cooling look very insignificant.
What's interesting is that the authors point out that climate change during the period may have helped to contribute to the eruption of the Toba.
What I have seen mentioned again and again in my research on the Ice Age Floods is that during the recession of Glaciers there is the risk of great seismic activity because of Isostatic Lift. As the crust re-bounds, being freed of the weight of the ice, there are more avenues for magma to release into the lithosphere and there are more opportunities for subduction and resultant earthquakes and volcanos.
In fact it is the probable seismic activity created by isostatic lift (resulting from the melting of Glaciers and lifted weight) that speeds up the ice melt and creates the large (comparitively speaking) reserviors of meltwater. In turn, as ice dams melt these volumes of meltwater are released and could be very disruptive for any mammals, etc in the area!
Volcanic winter and accelerated glaciation following the Toba super-eruption
Michael R. Rampino*† & Stephen Self‡
* Earth Systems Group, Applied Science Department, New York University, New York, New York 10003, USA
† NASA, Goddard Institute for Space Studies, New York, New York 10025, USA
‡ Department of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA
THE eruption of Toba in Sumatra 73,500 years ago was the largest known explosive volcanic event in the late Quaternary1. It could have lofted about 1015 g each of fine ash and sulphur gases to heights of 27–37 km, creating dense stratospheric dust and aerosol clouds. Here we present model calculations that investigate the possible climatic effects of the volcanic cloud. The increase in atmospheric opacity might have produced a 'volcanic winter'2—a brief, pronounced regional and perhaps hemispheric cooling caused by the volcanic dust—followed by a few years with maximum estimated annual hemispheric surface-temperature decreases of 3–5 °C. The eruption occurred during the stage 5a-4 transition of the oxygen isotope record, a time of rapid ice growth and falling sea level3. We suggest that the Toba eruption may have greatly accelerated the shift to glacial conditions that was already underway, by inducing perennial snow cover and increased sea-ice extent at sensitive northern latitudes. As the onset of climate change may have helped to trigger the eruption itself4, we propose that the Toba event may exemplify a more general climate–volcano feedback mechanism.
From
http://www.nature.com/nature/journal/v359/n6390/abs/359050a0.html
Sort of makes human influences on "global warming" or cooling look very insignificant.
What's interesting is that the authors point out that climate change during the period may have helped to contribute to the eruption of the Toba.
What I have seen mentioned again and again in my research on the Ice Age Floods is that during the recession of Glaciers there is the risk of great seismic activity because of Isostatic Lift. As the crust re-bounds, being freed of the weight of the ice, there are more avenues for magma to release into the lithosphere and there are more opportunities for subduction and resultant earthquakes and volcanos.
In fact it is the probable seismic activity created by isostatic lift (resulting from the melting of Glaciers and lifted weight) that speeds up the ice melt and creates the large (comparitively speaking) reserviors of meltwater. In turn, as ice dams melt these volumes of meltwater are released and could be very disruptive for any mammals, etc in the area!
Last edited: