Extinction motors

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Volcanic activity

For most of us, volcanoes are spectacles seen on television or referred to in books. There are about 1500 active volcanoes today of which about 80 are under the sea.

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You will notice that most of the active volcanoes occur where plates are colliding and resistance creates high pressure.

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The environmental damage caused by volcanoes is not limited to local lava flows and the widespread distribution of ash, but the emission of several toxic chemicals can have long-term global effects.
The massive Toba volcanic eruption26 in Sumatra about 73,000 years ago was so catastrophic that it may have caused a reduction of 5ºC in the average global temperature for several years and have initiated an ice age. Ash from the huge explosion was deposited 15cm thick over the whole of India and much of South East Asia. Parts of Malaysia were covered by nine metres of ash. Very few animals would have survived this and many species may have become extinct. It is believed that the world human population of the time was reduced by 60% to about 10,000 to 20,000 individuals by this disaster.

One volcanic event deserves special mention. The Deccan Traps are a large igneous province located on the Deccan Plateau of west-central India and one of the largest volcanic features on Earth. They consist of multiple layers of solidified flood basalt that together are more than 2,000 m thick and cover an area of 500,000 km². They were formed between 60 and 68 million years ago at the end of the Cretaceous period. The main bulk of the volcanic eruption occurred at the Western Ghats (near Bombay) some 66 million years ago and this series of eruptions may have lasted fewer than 30,000 years. The release of volcanic gases during the formation of the traps contributed to an apparently massive global warming. Some data point to an average rise in temperature of 8°C (14°F) in the last half a million years before the asteroid impact at Chicxulub. Deccan.jpg - 21504 Bytes