[meteorite-list] Study shows how impact craters may form
From: Sterling K. Webb <sterling_k_webb_at_meteoritecentral.com>
Date: Sat, 17 Dec 2011 15:13:41 -0600 Message-ID: <DC2E2E42B45A40EF8DD08D9E7220C079_at_ATARIENGINE2> Thanks, Paul. As is usual in science reporting, the "punch-line" is never explicit. If loosely compacted impactors make bowls and tightly compacted impactors make central peaks, what are these types most likely to correspond to in the real universe? Asteroids in general are less compacted than terrestrial materials because they form in weaker gravitational fields, but no doubt heading the list of tightly compacted materials are the irons. At Meteor Crater, Arizona, the iron impactor had already fragmented before it hit (or so they think). I would go even further out on that limb by guessing that bodies with an atmosphere (like Mars) might well have fewer central peak craters then airless bodies (like the Moon). I say "guess" because I'm not going to sit down and count them! Well, there's Google... 1966 study: http://articles.adsabs.harvard.edu//full/1977LPI.....8..181C/0000181.000.html says there's more central peaks on Mercury than the Moon which has, in turn, more central peaks than Mars. I would expect more iron impactors in the refractory zone around Mercury than out here around the Earth and Moon, and apparently Mars' atmosphere does protect it. All this seems to confirm the result. Going down the list are the more solid rocks followed by weaker rocks (like carbonaceous stones). Some asteroids are "rubblepiles" and have lots of internal voids. Eros and Itokawa are made of the same rock but Itokawa is far less dense, indicating that porosity and voids are present The weakest impactors would be likely be the comets (or any icy body whether you call it a comet or not). Sterling K. Webb --------------------------------------------------------------- ----- Original Message ----- From: "Paul H." <oxytropidoceras at cox.net> To: <meteorite-list at meteoritecentral.com> Sent: Saturday, December 17, 2011 8:36 AM Subject: [meteorite-list] Study shows how impact craters may form > Study shows how impact craters may form > http://dalje.com/en-world/study-shows-how-impact-craters-may-form/390016 > > Study shows how impact craters may form. Science News. > http://www.upi.com/Science_News/2011/10/20/Study-shows-how-impact-craters-may-form/UPI-26051319150854/#ixzz1cgD4itIS > > Crater shapes, UPI > http://www.upi.com/story/image/fs/UPI-26051319150854/13191492262400/ > > F. Pacheco- Vazquez and J. C. Ruiz- Suarez, 2011, Impact > craters in granular media: Grains against grains. Physical > Reviews Letters. vol. 107, no. 218001, 5 pp > http://prl.aps.org/abstract/PRL/v107/i21/e218001 > > Happy Holidays, > > Paul H. > ______________________________________________ > Visit the Archives at > http://www.meteoritecentral.com/mailing-list-archives.html > Meteorite-list mailing list > Meteorite-list at meteoritecentral.com > http://six.pairlist.net/mailman/listinfo/meteorite-list Received on Sat 17 Dec 2011 04:13:41 PM PST |
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