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Could We Survive An Asteroid Hit?
BBC News
4-14-4
 
An iron asteroid 20 metres (65.6ft) wide crashed into the Arizona desert 49,000 years ago, creating a crater a mile wide and 174m (570ft) deep.
 
The blast sent 175 million tons of rock flying into the air and whipped up winds of 1,000km (621 miles) per hour.
 
The effects on life in the region were devastating - but what impact would a similar blast have on a modern city such as London?
 
Scientists in the US have created a website to help us assess the risks.
 
According to researchers at the University of Arizona's Lunar and Planetary Laboratory, a relatively modest sized asteroid of 45m (148ft) in diameter hits the Earth approximately every 1,000 years.
 
So what would happen if the next one were to land in central London? How far would the devastation reach and how much time would those living and working in the city have to grab their bags and run?
 
To help assess the risks, University of Arizona researchers have created a website to help predict the effects of different types of asteroids and meteors would have if they hit different places on the planet.
 
Gigantic fireball sets trees alight
 
To use the site, you have to have an idea of what type of object you are expecting to hit the Earth, where it will hit and at what kind of speed and angle.
 
Simply type in your distance from the predicted impact point and the Earth Effects Impact Programme will tell you if you should expect to be buried under a pile of debris, known as ejecta, while trees are flattened for miles around or whether the effects will be limited to loud noises and rocking cars.
 
The site includes descriptions of the effects of different types of impacts, including how much thermal radiation is needed to ignite grass and how far away from the impact humans would suffer second or third-degree burns.
 
Planetary scientist Jay Melosh, who helped develop the site, said: "The website is valuable for scientists because they don't have to spend time digging up equations and data needed to calculate the effects.
 
"Similarly, it makes the information available to reporters and other non-scientists who don't know how to make the calculations."
 
The Arizona asteroid, thought to have been made of iron, hit the Earth at a 90% angle at a speed of 20km (12.4 miles) per second.
 
Inserting these figures into the online blast calculator for a slightly bigger iron asteroid of 45m (148ft) wide reveals devastating results should such an object hurtle into central London, landing say, at Oxford Circus.
 
An enormous crater 2.91km (1.81 miles) wide would spread across what had been Oxford Street, Bond Street, Regent Street and Marble Arch, wiping out much of Soho and Mayfair and sending hundreds of tons of rock hurtling into the air.
 
The immediate area would be vaporised instantly - the shoppers and officer workers thronging the streets would not stand a chance.
 
Rock thrown up by the blast would shower over an area of several square miles around the crater like bombs, smashing through the roofs of embassy buildings in Belgravia and skyscrapers in the City of London.
 
Just 0.04 seconds after the blast, a gigantic fireball, 0.8km (0.5 miles) across would appear, igniting trees, grass, paper and clothing, with thermal radiation causing extensive third degree burns in anyone unlucky enough to be caught within 1km of the blast .
 
A fraction of a second later, shockwaves from the blast would reach 5.4 on the Richter Scale, rocking cars up to 1km away, moving furniture, cracking walls and making the ground unstable to walk on. Widespread panic would likely ensue, with those who were able to running out of their houses into the streets.
 
Seismic shocks felt 60 miles away
 
The shockwaves would gradually spread out from the impact zone, reaching the London outskirts and the M25 about a second later.
 
Finally, 3.3 seconds after the impact, winds reaching 4,007km (2489.7miles) per hour will rush through the city, at an ear-piercing 128 decibels, causing buildings and bridges to collapse, steel-framed office blocks to buckle and blowing down 90% of the trees.
 
Seismic shocks would reach the M25 after about four seconds, rocking the ground, making it hard to stand up, church bells would ring and furniture would be overturned.
 
Even this far from the impact point, the fireball would be visible, cars and lorries would be destroyed, glass would be shattered and trees blown down and stripped of leaves by winds of 136km (84.6 miles) per hour.
 
The fireball following the impact would still be visible by people almost 100km (60 miles) away in Sussex, Essex or Hertfordshire, though the effects here would be milder.
 
Although cars may still be rocked by seismic shaking 19 seconds after the blast, the winds will reach only 23km (14.4 miles) per hour and will be no louder than heavy traffic noise.
 
© BBC MMIV http://news.bbc.co.uk/2/hi/science/nature/3622183.stm


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