Vanadium 50 said:
You haven't posted a new meteorite in 3 weeks...are you OK?
Hi ya,
Yes, still kicking. I have had 2 new postal arrivals and there are 3 more parcels on the way.
Hopefully one of those 3 I will see this coming week
The 2 that arrived one was from Brett, a seller in PA state of the USA
Top left was a gift he included 3 fossil teeth left to right
L -- Hemipristis is a genus of weasel sharks, family Hemigaleidae. It contains one extant species, the snaggletooth shark (H. elongata) and several extinct species. Hemipristis has two distinct types of teeth in each section of its jaw.
M -- Tiger Shark tooth -- The tiger shark is a species of requiem shark and the only extant member of the genus Galeocerdo.
It is a large macropredator, capable of attaining a length over 5 m.
R -- Stingray tooth - I don't know which species
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Top right is a new meteorite find ( but an old fall) the Erg Chech 002 from the desert area of SW Algeria.
One of the things that indicate an old fall is the total lack of fusion crust on any of the material found. It has long ago been eroded off. This meteorite was only classified ~ 4 weeks ago as an Achondrite-ungrouped. The Meteoritical Bulletin entry ...
https://www.lpi.usra.edu/meteor/metbull.php?sea=Erg+Chech+002&sfor=names&ants=&nwas=&falls=&valids=&stype=contains&lrec=50&map=ge&browse=&country=All&srt=name&categ=All&mblist=All&rect=&phot=&strewn=&snew=0&pnt=Normal table&code=72475
This an exciting new find as the meteorite is so very different to any other one because of its visual appearance colour and mineral content.
Many seasoned collectors have said " had they seen this rock without knowing that it was a meteorite, they would have said it wasn't one"
It contains distinguishing long green - yellow crystals of diopside ( a pyroxene)
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The lower meteorite is The Tassedet 004, an H5 melt breccia
explanation ...
Ordinary chondrite: A major class of chondrites, distinguished by sub-solar Mg/Si and refractory/Si ratios, oxygen isotope compositions that plot above the terrestrial fractionation line, and a large volume percentage of chondrules, with only 10-15 vol% fine-grained matrix.
H group: The high-iron (H) chemical group of ordinary chondrites, distinguished by their high siderophile element content, relatively small chondrules (~0.3 mm), and oxygen isotope compositions that are closer to the terrestrial fractionation line than those of other ordinary chondrites.
Type 5: Designates chondrites that have been metamorphosed under conditions sufficient to homogenize olivine and pyroxene,
convert all low-Ca pyroxene to orthopyroxene, cause the growth of various secondary minerals, and blur chondrule outlines.
Melt breccias come from all 3 known sources of meteorites, Lunar, Martian and the asteroids and are caused my impacts... asteroid - asteroid and asteroid to Moon or Mars
Vanadium 50 said:
What is a UNWA compared to a regular NWA and why are they 10x cheaper?
Unclassified meteorites from NWA and other places are cheaper because they are unclassified.
The obvious features can be stated, eg. it's a chondrite, anchondrite or a melt breccia and estimates can be made to its metal content classification H = high iron, L = low iron etc. But unless a sample
was actually taken to a lab for chemical analysis, the fine details cannot be confirmed.
cheers
Dave