Eucrites

The Eucrites are named for a Greek word meaning "easily distinguished". Representing the most common class of achondrites, more than 100 eucrites are known, excluding all probable pairings. Although they are easily distinguished from chondrites, they closely resemble terrestrial basalts. Actually, eucrites are extraterrestrial basalts, volcanic rocks of magmatic origin, representing the crust of their parent body, Vesta. They are primarily composed of the calcium-poor pyroxene, pigeonite, and the calcium-rich plagioclase, anorthite. Additionally, eucrites often contain accessory minerals such as silica, chromite, troilite, and nickel-iron metal. Based on mineralogical and chemical differences, the eucrites have been further divided into three distinct subgroups: the non-cumulate group, the cumulate group, and the polymict group.

Bereba Fell June 27, 1924, Upper Volta TKW 18 kg Monomict eucrite Highly shocked
Bereba 00 Big endcut with shinning fusion crut 168 gr Price on request
				Bereba 01 Nice endcut with shinning fusion crust, a killer specimen !! 26.62 gr Price on request
Bereba 02 Big slice with shocks veins  25.76 gr SOLD
				Bereba 03 Small slice with shocks veins  0.992 gr SOLD
Bereba 04 Small endcut with shocks veins  0.672 gr $ 120
				Bereba 05 Small slice with shocks veins  0.670 gr SOLD
Bereba 06 Small slice with shocks veins  0.392 gr $ 80
				Bereba 07 Small fragment with shocks veins  0.412 gr $ 80
Bereba 08 Small fragment with shocks veins 0.444 gr $ 80