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.

Millbillillie Fell 1960, Western Australia TKW 330 kg Polymict Eucrite
Millbillilie 000 perfect individual crusted ! 135.32 gr SOLD
				Millbillillie 00 perfect individual 135gr $3375
Millbillilie 01 perfect individual from the C.Sthelin collection 72gr $1800
				Millbillillie 02 crusted end cut, face polished 18.90gr Price on request
Millbillilie 03 crusted half individual 13.65gr SOLD
				Millbillillie 04 crusted half individual 12.57gr SOLD
Millbillilie 05 crusted half individual 12gr SOLD
				Millbillillie 06 crusted half individual, grey matrix 5.57gr $140
Millibillillie 03 crusted half individual 4.56gr $115