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Asteroid impact simulator

Mark Frauenfelder at 12:38 pm Wed, Nov 14, 2012

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Ben Winters, author of The Last Policeman (which I reviewed here), sent me a link to a website called Impact Earth! It was developed by Gareth Collins, HJ Melosh, and Robert Marcus at Purdue University. To use it, you enter parameters about the size and density of the hypothetical asteroid, the impact angle, the distance from impact, etc.

What happens when a rock the size of a school bus hits the Earth at an angle of 45° and a speed of 40 km/s? According to Impact Earth!

The projectile bursts into a cloud of fragments at an altitude of 96,500 ft.

No crater is formed, although large fragments may strike the surface.

Energy before atmospheric entry = 544.05 KiloTons TNT.

The average interval between impacts of this size somewhere on Earth is 68.8 years.

That's reassuring! What about a much larger astroid, say 1.3 km in diameter?

Energy before atmospheric entry: 6.6 x 10^5 MegaTons TNT

The average interval between impacts of this size somewhere on Earth during the last 4 billion years is 3.3 x 10^6 years

Final Crater Diameter: 16.7 miles

Final Crater Depth: 2610 feet

Mercalli Scale Intensity at a distance of 10 km: Most masonry and frame structures destroyed with their foundations. Some well-built wooden structures and bridges destroyed. Serious damage to dams, dikes, embankments. Large landslides. Water thrown on banks of canals, rivers, lakes, etc. Sand and mud shifted horizontally on beaches and flat land. Rails bent slightly. Underground pipelines completely out of service.

Getting bigger, a 50-kilometer asteroid will make a final crater 603 miles wide and 1.46 miles deep. If you are within 1000 kilometers of the point of impact you will be inside the resulting fireball, which will hit you 37.4 seconds after impact. Fortunately, "the average interval between impacts of this size is longer than the Earth's age. Such impacts could only occur during the accumulation of the Earth, between 4.5 and 4 billion years ago."

Asteroid impact simulator

Mark Frauenfelder is the founder of Boing Boing and the editor-in-chief of MAKE and Cool Tools. Twitter: @frauenfelder. Come and hear Mark speak at the ALA conference in Chicago on July 1.

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  • http://twitter.com/nagmay Gabriel Nagmay

    But, what if it’s made of diamond and traveling at (near) the speed of light?
    http://what-if.xkcd.com/20/

    • cellocgw

      Ahh, ya beat me to it :-)

  • Paul Renault

    Why not just use the closing scenes from Nuclear War, discussed earlier..
    https://en.wikipedia.org/wiki/Nuclear_War_%28video_game%29

  • Florian Bösch

    The Earth is completely disrupted by the impact and its debris forms a new asteroid belt orbiting the sun between Venus and Mars.
    100 percent of the Earth is melted.

    I may have went a wee overboard with the size, also with the velocity, possibly the density doesn’t really matter at that point.

  • blissend

    Anyone else able to create a tsunami? Having more trouble than I thought one should when creating massive craters are so easy.

  • David Kopelman

    Absolutely the best app ever for a Nihilist. I created a tsunami 1950 ft high! 

    “Your position is beneath the continuous ejecta deposit.” Oh, that’s usually a bad thing.

  • oasisob1

    It doesn’t handle some inputs very well. I obtained results with craters 2300000 km wide, day shifts of 11000 hours (described as not significant)…

  • Aaron Ximm

    What I learned(?): the asteroid Maia aka 2011GV1 in ‘The Last Policeman’ is not necessarily an extinction level or (it seems) a civilization-ending event.

    True, the simulator doesn’t talk about ‘nuclear winter’ style climate effects as such… but still. Oops?

  • http://twitter.com/tueksta Andreas Beer

    “The impact-generated tsunami wave arrives approximately Infinity hours after impact.” could use some finetuning…

  • http://profile.yahoo.com/5B7YN32JIIITSH7PIBMJ3NBUII ivan

    At half the speed of light a ping pong ball (40mm in diameter:2,7 grams) will have the same kinetic energi as the moon. Auch.