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'By far the greatest danger of Artificial Intelligence is that people conclude too early that they understand it'

 

Eliezer Yudkowsky

Asteroid strike made 'instant Himalayas'

RATE THIS! +27
Posted in Science on 19th Nov, 2016 12:15 PM by AlexMuller

Scientists say they can now describe in detail how the asteroid impact that wiped out the dinosaurs produced its huge crater. The reconstruction of the event 66 million years ago was made possible by drilling into the remnant bowl and analysing its rocks. These show how the space impactor made the hard surface of the planet slosh back and forth like a fluid.

 

At one stage, a mountain higher than Everest was thrown up before collapsing back into a smaller range of peaks. "And this all happens on the scale of minutes, which is quite amazing," Prof Joanna Morgan from Imperial College London, UK, told BBC News. The researchers report their account in this week's edition of Science Magazine.
 
Their study confirms a very dynamic, very energetic model for crater formation, and will go a long way to explaining the resulting cataclysmic environmental changes.
 
The debris thrown into the atmosphere likely saw the skies darken and the global climate cool for months, perhaps even years, driving many creatures into extinction, not just the dinosaurs.
 
The team spent May to June this year drilling a core through the so-called Chicxulub Crater, now buried under ocean sediments off Mexico's Yucatan Peninsula.
 
The analysis of the core materials now fits an astonishing narrative. This describes the roughly 15km-wide stony asteroid instantly punching a cavity in the Earth's surface some 30km deep and 80-100km across.
 
Unstable, and under the pull of gravity, the sides of this depression promptly started to collapse inwards. At the same time, the centre of the bowl rebounded, briefly lifting rock higher than the Himalayas, before also falling down to cover the inward-rushing sides of the initial hole.
 
"If this deep-rebound model is correct (it's called the dynamic collapse model), then our peak ring rocks should be the rocks that have travelled farthest in the impact - first, outwards by kilometres, then up in the air by over 10km, and back down and outwards by another, say, 10km. So their total travel path is something like 30km, and they do that in under 10 minutes," Prof Gulick told the BBC's Science in Action programme.

Tags: asteroidrockgeologyresearch

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