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The Eruption of Mt. Pinatubo: Volcanoes and the Oceans There are a number of anti-environmentalists who assert, among other things, that the impacts of climate change and global warming are fabrications of extreme environmentalism. Media personality Rush Limbaugh repeatedly asserts that natural phenomena like volcanic eruptions emit pollutants in volumes such as to dwarf those produced by human activity, thus "proving" that fears of global climate change are fabricated. One way to evaluate the basis for that claim is to assess the impact on the earth's atmosphere of the eruption of a large volcano. Although there are hundreds of active volcanoes worldwide, most erupt only intermittently. A few massive eruptions have occurred during the past several thousand years, like Mt. Mazama in Oregon, whose remains make up Crater Lake National Park. Once every few hundred thousand years, a truly gigantic eruption occurs, producing deposits like Californias Bishop Tuff, with profound local and regional effects on climate and life. Our concern here is with the potential long-term impact of volcanic eruptions. Do they in fact emit greenhouse gases and SO2 in amounts to swamp those from human activities? The eruption of Mt. Pinatubo in the Philippines was the second largest volcanic eruption of the twentieth century, dwarfing Mt. St. Helens in mass of emitted material. The 1980 eruption of Mount St. Helens had a Volcano Explosivity Index (VEI) of 5. (There have been 84 known eruptions of VEI=5 in the last 10,000 years). The eruption produced 1 billion cubic meters of ash and 10 million cubic meters of lava. The 1991 eruption of Pinatubo had a Volcano Explosivity Index of 6. (There have been 39 known eruptions of VEI=6 in the last 10,000 years). The eruption produced 10 billion cubic meters of ash. If any natural event could be targeted as a major source of CO2 Pinatubo should be it. Things you need to know: Important conversions The density (mass per unit volume) of volcanic material ranges from less than 1,000 kg/m3 for pumice and ash to nearly 3,000 kg/m3 for some basalts. A high average for Mt. Pinatubo is 2,000 kg/m3, since most of it was ash.
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