Until I bring this specimen down to UCLA, Have a Happy Holiday!
Bob V.
P.S. - Here are some images of my "meteor-wrong FIND(?)".
This one shows its general ORIENTED shape:
<
https://meteorite-recovery.tripod.com/studyarea3/radl-203.jpg>
This one shows the FUSION CRUST:
<https://meteorite-recovery.tripod.com/studyarea3/radl-212.jpg>
This one shows FLOW-LIPPING of the "fusion crust" as it accumulates on the back side of the "oriented" mass:
<https://meteorite-recovery.tripod.com/studyarea3/radl-205.jpg>
The "fusion crust" exhibits CONTRACTION CRACKS:
<https://meteorite-recovery.tripod.com/studyarea3/radl-223.jpg>
The back side of the "oriented" mass is not crusted over and exhibits small, spheroidal pseudo-CHONDRULES:
<https://meteorite-recovery.tripod.com/studyarea3/radl-222.jpg>
This is the URL for a directory containing additional images:
<https://meteorite-recovery.tripod.com/studyarea3/>
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--- Paul Warren <pwarren@ucla.edu> wrote: > Bob, > > I saw the pictures. The stone looks weird, all > right. The odds are always in favor of terrestrial > provenance, and I presume you know that desert > varnish can sometimes do a mighty impressive > imitation of fusion crust. Yes, this is very true. In fact, I have some excellent examples of desert varnish in my meteor-wrong collection. > However, I don't see why you are so positive it can't > be a meteorite. > Is it magnetic? No magnetic attraction can be discerned. > How does its density compare with typical terrestrial > rock such as granite? Nearly half that of non-porous terrestrial granitic rock. (My main counter-indication.) > The only counter-indication I saw was the contraction cracks > (I've never heard of such a thing on a true meteorite, > although that does not necessarily rule it out). Please excuse my terminology. There must be a better term for what I'm trying to describe, because I've seen these "cracks" exhibited in many different meteorites. (But come to think of it, I can only remember seeing it in small chondritic stones.) Here's one of my first introductions to this phenomenon of "contraction cracks" - Lucerne Valley 014 (L5): <https://members.tripod.com/~beaulide/lucerne/ldl-1st.htm> Here's LV 010 (H4): <https://members.tripod.com/~bolidechaser/grifith2/MVC-013F.JPG> Here's Muroc Dry Lake (L6): <https://members.tripod.com/~bolidechaser/grifith3/mroc-dl3.jpg> Here's Muroc (L5): <https://members.tripod.com/~bolidechaser/grifith3/muroc-03.jpg> NOTE: The last time that I thought I had found a piece of partially burnt model rocket propellant, but turned out to be a chondrite, was the LL6 known as Lucerne Valley 015 ;-) <https://members.tripod.com/~bolidechaser/lucerne/lv015-p1.htm> > Happy Holidays! > > Paul Have a Happy One, yourself! Bob V.