This meteorite was recovered out of Morocco in 2003 and was analyzed by Dr. Ted Bunch at NAU. It was classified and determined to be a brecciated howardite with unusual characteristics. This fresh howardite has been held in a private collection and has not been available on the collector market in many years.
The specimen being offered here is a lot. It is a capsule filled with small fragments and dust from the cutting process. This would be ideal for destructive analysis or other scientific research purposes. The contents of the capsule weigh approx. 1.26 grams and consists of a mix of small solid fragments, fusion crust chips, and fine cutting dust.
Refer to the photo. The black centimeter cube is shown for scale and is not included. You are purchasing the capsule shown. Your purchase will include a labeled gemjar for safe storage.
From the Meteoritical Bulletin entry on NWA 2060 :
Northwest Africa 2060
A 985 g, very fresh stone with shiny fusion crust, was purchased in Rissani, July 2003. Classification and mineralogy (T. Bunch and J. Wittke, NAU): a howardite of unusual characteristics. Fine-grained and powdery, average clast and mineral grain size is < 2 mm with few clasts > 3 mm. Clast modes: diogenites, 74 vol. %; eucrites 20 vol. % (12 % cumulate, 8 % basaltic); anorthositic-like clasts, 3 %; shock melt clasts. 2 %, and opaques, 1%. Diogenite orthopyroxene, Fs35.6-38.8Wo2.3-4.2; plagioclase, An 87; chromite, Cr/(Cr+Al) = 0.81; metal, Ni = 0.67 wt %. Melt inclusions in opx contain Ca-rich pyroxene, Fs33.3Wo37.5; phosphate, silica phase, and K-rich glass. Plagioclase-pyroxene cumulates, Fs38.2Wo21; plagioclase, An86.Other eucrite textures include recrystallized, granular, ophitic, subophitic, and variolitic (Fs31.6Wo7 and Fs61.8Wo33). Plagioclase-rich clasts have 95 vol.% plagioclase (An96.1). Mildly shocked; no apparent oxidation or Fe staining. Specimens: 26 g, NAU: main mass. Boswell.