138g individual. Dimensions : 5.5 x 6.1 x 3.1 cm. Sold with label/certificate of authenticity.
Bassikounou is the perfect exemple of a recent meteorite fall which remained unknown to the public for several months before its discovery. In fact, the strewnfield is located in an extremely remote area where poor populations which don’t have access to modern communication technologies live. I highly recommend the report published by the german meteorite hunter Svend Bühl. You can read it at http://www.meteorite-recon.com
Mauritanian newspaper Horizons (october 23 to 26, 2006) published a short report of the fall : « The inhabitants of the wilaya of Hodh Echargh observed on october 16, 2006 in the evening the fall of a bright bolide which lit the most part of the wilaya, particularly from Nema to Bassiknou. Administrative and military authorities of the wilaya went at the place of fall and reported that a large meteorite had fallen at 17 km from Bassiknou and dug a large ditch and they took some fragments for its study. »
Bassikounou 15°47’N, 5°54’W
Bassikounou, Hodh Ech Chargui, Mauritania
Fall: 16 October 2006; 04:00 UTC
Ordinary chondrite (H5)
History: A fireball was witnessed in the area, but no records of the direction of movement were recorded. A single stone of 3165 g was found by A. Salem El Moichine, a local resident, on the same day at 13:00 hr local time, 11 km SE of Bassikounou. The sample for classification was provided to NMBE by M. Ould Mounir, Nouakchott, who obtained it from his cousin who recovered the meteorite. According to S. Buhl (Hamburg, Germany), more than 20 specimens were later recovered by locals and meteorite finders. These finds define a 8 km long strewnfield. The total recovered mass is 46.00 kg.
Physical characteristics: The 3165 g specimen is largely covered by black fusion crust. The interior is light gray. On the surface of the fusion crust there is some adherent soil material, some of which is bright red. Shortly after recovery, the stone was cut into two pieces of 1200 and 1950 g. The larger piece has a rectangular shape and shows indications of flow-lines in the fusion crust.
Petrography: (E. Gnos, MHNGE; B. Hofmann, NMBE, M. Eggimann, Bern/NMBE): Mean chondrule size 0.35 mm (n=53). Metal abundance is 8 vol%, troilite 6.6 vol%. Mean plagioclase grain size is ~20 mm. Troilite is polycrystalline, rich in silicate inclusions, and shows diffuse boundaries to metal. Metal is partly rich in silicate- and troilite inclusions. Rare metallic Cu (10 mm) occurs at kamacite-taenite boundaries and in troilite. Some shock veins and no weathering products were observed.
Mineral compositions: Olivine (Fa18.6), pyroxene (Fs16.3 Wo1.1), plagioclase (An13.7).
Cosmogenic radionuclides: (P. Weber, PPGUN) Gamma-spectroscopy performed in December-January 2006 showed the presence of the following radionuclides: 48V, 46Sc, 56Co, 54Mn, 58Co, 7Be, 51Cr, 57Co, 22Na, 26Al and 60Co. Recalculated to 12 October 2006 22Na was 38.0±2.2 and 26Al 31.5±2.1 (both dpm/kg), the activity ratio of 1.21 is fully consistent with a fall on that date.
Classification: Ordinary chondrite (H5); S2, W0.
Type specimens: A total of 115 g are on deposit at NMBE. Boudreaux holds the main mass.