The Tamdakht meteorite fell near Ouarzazate, Morocco on 20 December 2008 producing a strewn field of approximately by and two small impact craters, one of about diameter and depth at and the other of about diameter and depth at .
The meteorite is named after a village close to the fall.
On April 22, 2017, small bits of the meteorite were handed out to children at the Boston March for Science.
Petrology: (by Albert Jambon, Omar Boudouma, D. Badia UPVI and M. Denise, MNHNP): Abundant chondrules with visible but not well-delimited outlines. Chondrule size is 0.1 to 1.5 mm. Dominant olivine and orthopyroxene. Abundant chromite, rare clinopyroxene and ilmenite. Numerous pockets with chromite, plagioclase and phosphate (merrilite and Cl-apatite). Kamacite, with deformed Neumann bands, and taenite, twinned troilite. Copper. Mode: metal+troilite 10%.
Mineral compositions and geochemistry: log à= 5.3. Olivine Fa18 ñ 0.5 Opx = En83 Fs16 Wo2 Minor calcic pyroxene. Plagioclase is Ab83âÂÂ86 An5âÂÂ15 Or7âÂÂ2. Ca-phosphate (merrillite and Cl-apatite). Chromite: Cr# (100àmolar Cr/[Cr + Al]) = 82. Metal: kamacite with 5% Ni and taenite with 36âÂÂ47% Ni. Oxygen isotopes (C. Suavet, J. Gattacecca CEREGE): ô17O = 3.26â°, ô18O = 5.01â°, and ÃÂ17O = 0.65â°. Magnetic susceptibility is log à= 5.3 à10âÂÂ9 m3/kg.
Ordinary chondrite (H5), S3, W0.