Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!utgpu!water!watnot!watmath!clyde!rutgers!seismo!ll-xn!cit-vax!oddhack!jon From: jon@oddhack.UUCP Newsgroups: sci.bio,sci.astro Subject: Re: Mass extinctions Message-ID: <2330@cit-vax.Caltech.Edu> Date: Mon, 13-Apr-87 17:49:58 EST Article-I.D.: cit-vax.2330 Posted: Mon Apr 13 17:49:58 1987 Date-Received: Wed, 15-Apr-87 03:36:28 EST References: <6760@alice.uUCp> <1489@kontron.UUCP> <1244@husc2.UUCP> <1510@kontron.UUCP> <2329@cit-vax.Caltech.Edu> Sender: news@cit-vax.Caltech.Edu Reply-To: jon@csvax.caltech.edu (Jon Leech) Organization: California Institute of Technology Lines: 39 Keywords: sanity check Xref: utgpu sci.bio:279 sci.astro:837 In article <2329@cit-vax.Caltech.Edu> fritz@polecat.Caltech.EDU (Fritz Nordby) writes: >>> In article <1489@kontron.UUCP>, cramer@kontron.UUCP (Clayton Cramer) writes: >>>> 1. No great surprise, but the estimates for one of the Canadian astroblemes >>>> is 17,500,000 megatons. (No, not 17.5 megatons -- 17.5 gigatons). > >Uh, gee, isn't that kind of large? >Assuming the creature was about as dense as water >I work out that these creatures must have had a >volume of >16500 cubic kilometers! >That's a cube of more than 25 kilometers on a side. No, this is eminently reasonable. A simple relation of impact energy to crater diameter derived by Shoemaker [1] is: 1/3.4 D(km) = K W where 1/3.4 K = 0.074 km / (kT TNT equivalent) W = kinetic energy of impact body, kT TNT equivalent so for a 17.5e12 T = 17.5e9 kT impact, a crater diameter of 76 km is obtained, which passes sanity checks. Note that this model is for alluvium, a main constituent of the earth at the Nevada nuclear test range where data for the model was developed; it scales weakly with the density of the material at the impact site. If the impact in question was on the Canadian shield, the predicted diameter would be somewhat smaller. The odd (1/3.4) exponent is more of a fit to observed explosions than a theoretical model. Geometry suggests that crater diameter goes as the 2/3 power of yield, but there are other factors involved. [1] Eugene Shoemaker & Ruth Wolfe, ``Cratering Time Scales for the Galilean Satellites'', in Satellites of Jupiter, ed. David Morrison, Univ. of Arizona press 1982. The actual model was developed elsewhere; this is just a reference which applies it. -- Jon Leech (jon@csvax.caltech.edu || ...seismo!cit-vax!jon) Caltech Computer Science Graphics Group __@/