This odd meteorite was marketed as a witnessed fall by the finders. It supposedly fell on June 8, 2014, but was not recovered until several months later. I spoke with Dr. Hasnaa Chennaoui about its analysis; she said that samples were being studied for short-lived radionuclides, and that it would be submitted as a witnessed fall if a recent date was confirmed.
The fusion crust on some samples appears to be completely unweathered, but others appear to show some sand-blasting (natural) indicative of a terrestrial age of some years. I am not certain if it will be called a fall or a find.
The rock itself is quite interesting. It is highly metamorphosed, with visible plagioclase grains as large as 2-3 mm visible on the surface of broken specimens. The mafic clasts appear waxy; I have never seen a meteorite quite like it. It has large troilite inclusions, which suggest that it is an LL chondrite. It will most likely be classified as a brecciated LL6 or LL7, depending upon the scientist who analyzes it. There is a small chance that it is achondritic and more closely related to diogenites.
A number of stones have been well-documented; below is a photo of one such stone.
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