Two stones (414 and 383 g) were found in the Atlas mountains

(Morocco) in 2001 January and March. The exact location of find

is unknown. The meteorite is a cumulate peridotitic rock consisting

of olivine (~ 55 vol%), low and high-Ca pyroxenes (~ 35

vol%) and plagioclase glass (~ 8 vol%). Accessory minerals include

phosphates (merrillite), chromite and spinels (inclusions in

olivines and pyroxenes), sulfides (pyrrhotite), and a glass rich in

potassium.The igneous texture is very similar to that of the

En78Fs19Wo2-En60Fs26Wo14, and augite, En53Fs16Wo31-

En45Fs14Wo41; maskelynite ranges from An57Ab41Or1 to

An40Ab57Or3. The key element weight-ratios FeO*/MnO is close

to 30 for pigeonite and close to 50 for olivines. Geochemistry:

REE pattern similar to that of ALHA77005 but with higher values.