Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!utgpu!water!watnot!watmath!clyde!rutgers!ames!cit-vax!oddhack!jon From: jon@oddhack.UUCP Newsgroups: sci.bio,sci.astro Subject: Re: Mass extinctions Message-ID: <2212@cit-vax.Caltech.Edu> Date: Fri, 3-Apr-87 03:47:34 EST Article-I.D.: cit-vax.2212 Posted: Fri Apr 3 03:47:34 1987 Date-Received: Sun, 5-Apr-87 02:27:25 EST References: <6760@alice.uUCp> <496@uokmax.UUCP> <3345@udenva.UUCP> Sender: news@cit-vax.Caltech.Edu Reply-To: jon@csvax.Caltech.EDU (Jon Leech) Organization: California Institute of Technology Lines: 14 Keywords: Iridium, Osmium, Ash Xref: utgpu sci.bio:222 sci.astro:800 In article <3345@udenva.UUCP> agranok@udenva.UUCP (Alexander Granok) writes: >One of the things that had bothered scientists was the evidence of the impact. >Something that large would leave visible scars for some time, wouldn't it? >Unless it landed in the ocean, which is an interesting idea which has recently Depending on the nature of the target material (shield rock lasts about the longest), large craters are eroded away on timescales on the order of ten million years. Any given impact is likely to have taken place in an area that is currently covered by water, anyway (after all, the Earth is ~70% oceans!) -- Jon Leech (jon@csvax.caltech.edu || ...seismo!cit-vax!jon) Caltech Computer Science Graphics Group __@/