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Large comet explosion 'caused earth's cooling 13,000 years ago'

By Super Admin
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Google Oneindia News

Washington, April 2 (ANI): Thousands of Tunguska-sized cometary fragments struck the earth for over an hour 13,000 years ago, leading to a dramatic cooling of the planet, according a new study.

The cooling, by as much as 8 degrees Celsius, interrupted the warming which was occurring at the end of the last ice age and caused glaciers to readvance.

"A large comet has been disintegrating in the near-Earth environment for the past 20,000 to 30,000 years, and running into thousands of fragments from this comet is a much more likely event than a single large collision," said Bill Napier, professor at the Cardiff University Astrobiology Centre, who conducted the study.

Evidence has been found that this catastrophic change was associated with some extraordinary extraterrestrial event.

These findings suggest that the catastrophic changes were caused by the impact of an asteroid or comet four km across on the Laurentide ice sheet, which at that time covered what would become Canada and the northern part of the US.

The cooling lasted over a thousand years, and its onset coincides with the rapid extinction of 35 genera of North American mammals, as well as the disruption of the Palaeoindian culture.

The chief objection to the idea of a big impact is that the odds against the earth being struck by an asteroid this large only 13,000 years ago are a thousand to one.

Napier has now come up with an astronomical model, which accounts for the major features of the catastrophe without involving such an improbable event.

The new model indicates that such an encounter would last for about an hour during which thousands of impacts would take place over continental dimensions, said a Cardiff release.

Each of these impacts released the energy of a megaton-class nuclear bomb, generating the extensive wildfires, which took place at that time.

The new model has been presented in the journal Monthly Notices of the Royal Astronomical. (ANI)

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