Hi All again, It seems that my link didn't work; let me try again, actually I have several pictures:
http://meteoriteshow.free.fr/images/for_sale/July_2007/Benguerir/benguerir-7 9.6g(1).jpg http://meteoriteshow.free.fr/images/for_sale/July_2007/Benguerir/benguerir-7 9.6g(7).jpg http://meteoriteshow.free.fr/images/for_sale/July_2007/Benguerir/benguerir-7 9.6g(6).jpg http://meteoriteshow.free.fr/images/for_sale/July_2007/Benguerir/benguerir-7 9.6g(3).jpg Cheers Fred www.meteoriteshow.com IMCA #2491 -----Message d'origine----- De : meteorite-list-boun...@meteoritecentral.com [mailto:meteorite-list-boun...@meteoritecentral.com] De la part de Martin Altmann Envoyé : lundi 27 mai 2013 14:26 À : meteorite-list@meteoritecentral.com Objet : [meteorite-list] (House-AD): Two special Chelyabinsk individualswith Brown Lee-side Crust - color-oriented! Importance : Haute Hello there, we have to share with you a pretty exciting observation. It was here already on the list, that some of you found on the first-pick Chelyabinskis places with a brownish, nevertheless fresh fusion crust. That phenomenon btw. you had sometimes also on a few Tissints, there the brown crust was even translucent (were horribly difficult to sell, because people watching the photos were skeptical, thought, they wouldn't be fresh, but weathered - and that, where no iron is present in Tissint to rust). Many of you blossomed during the last 3 months into true Chelyabinsk-experts, so please, pay attention to those two individuals and tell us your opinion: 75.45g http://www.meteoritenhaus.de/img/Chelyabinsk_75_45_g_01.JPG http://www.meteoritenhaus.de/img/Chelyabinsk_75_45_g_02.JPG http://www.meteoritenhaus.de/img/Chelyabinsk_75_45_g_03.JPG 68.37g http://www.meteoritenhaus.de/img/Chelyabinsk_68_37_g_01.JPG http://www.meteoritenhaus.de/img/Chelyabinsk_68_37_g_02.JPG http://www.meteoritenhaus.de/img/Chelyabinsk_68_37_g_03.JPG http://www.meteoritenhaus.de/img/Chelyabinsk_68_37_g_04.JPG Well, baffling, aren't they? Both of them have a side, and ONLY one side, which is fully coated by the brown crust, while all other sides are black, as usual. Here: http://www.meteoritenhaus.de/img/Chelyabinsk_68_37_g_02.JPG And here: http://www.meteoritenhaus.de/img/Chelyabinsk_75_45_g_02.JPG And you see, that the brown-side is framed all around by a lipping, which is black, hence most would therefore say, only because of the rollover-lip, that the stones are flight-oriented. At least one can say, by means of the circular lipping around the edges, that the stones had for a longer time a stable position in flight. And that the brown side is the backside, the lee-side. And what is striking, is, that the lipping overlaps the brown crust, hence the brown crust must have formed simultaneously, while the front surface was melting. Now one could speculate, what could have caused that different crust - from the chip missing in one of the stones, we see that the material beneath the brown crust isn't special (anyway, on the sides the fusion crust for the same material is black). Thus maybe the different color could stem from a lack of oxygen, when it melted, on the lee-side of the stone in flight, where one has a low pressure/partial vacuum? We think, one could even speak of a new category of orientation: COLOR-ORIENTED! Well, if you like to have them, what shall we do with so special specimens... Let's make 20$/g to be among the very cheapest Chelyabinsk-offerers, + 50cents for the lipping, where others would scream: oriented, oriented! + 1.5$/g for the fantastic "color-orientation"... Makes 22$/g. Fascinating, aren't they? Your Meteorite House Team ______________________________________________ Visit the Archives at http://www.meteorite-list-archives.com Meteorite-list mailing list Meteorite-list@meteoritecentral.com http://six.pairlist.net/mailman/listinfo/meteorite-list ______________________________________________ Visit the Archives at http://www.meteorite-list-archives.com Meteorite-list mailing list Meteorite-list@meteoritecentral.com http://six.pairlist.net/mailman/listinfo/meteorite-list