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Originally posted by spikester
reply to post by smurfy
Tunguska's object was around three times larger. OP
Yeah maybe, could have much smaller just made of anti-matter. This is just the ones we know of, although the Gov. can detect things in space from small and near to far and huge. Lots of variables on object impact such as angle of entry, size of course, material and land or sea impact. some meteiors explode, burn up or just skip off the atmosphere. I'm no expert as you can tell, but study into this subject is facinating.
edit on 6-4-2011 by spikester because: (no reason given)
Originally posted by Illustronic
I ran a simulation of a 30 meter asteroid made up of dense rock, traveling 20 km/sec (typical speed), and entering at a 45º angle and this is the atmospheric results I got.
The projectile begins to breakup at an altitude of 56600 meters = 186000 ft
The projectile bursts into a cloud of fragments at an altitude of 15300 meters = 50100 ft.
The residual velocity of the projectile fragments after the burst is 10.3 km/s = 6.4 miles/s.
The energy of the airburst is 6.23 x 10^15 Joules = 1.49 x 10^0 MegaTons.
No crater is formed, although large fragments may strike the surface.
More on that;
The air blast will arrive approximately 5.11 minutes after impact.
Peak Overpressure: 845 Pa = 0.00845 bars = 0.12 psi
Max wind velocity: 1.98 m/s = 4.44 mph
Sound Intensity: 59 dB (Loud as heavy traffic)
You may not get all of the information you want, but you can play around with many variables at this site.
www.purdue.edu...