description Bereba Overview
Bereba is a eucrite meteorite that fell in present-day Burkina Faso in 1924. Eucrites are basaltic achondrites within the howardite-eucrite-diogenite group, recording igneous activity on a differentiated parent body widely associated with asteroid 4 Vesta. Bereba is therefore studied as extraterrestrial basalt rather than as a primitive, unmelted chondrite.
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Where and when did the Bereba meteorite fall?
The Bereba meteorite fell in present-day Burkina Faso in the year 1924. It was an observed fall that yielded a significant amount of material.
What is the scientific classification of the Bereba meteorite?
Bereba is classified as a eucrite, which is a type of basaltic achondrite. Eucrites are part of the broader howardite-eucrite-diogenite (HED) group of meteorites.
What is the parent body of the Bereba meteorite?
The HED group of meteorites, including Bereba, is widely believed to originate from the massive asteroid 4 Vesta. They represent igneous activity that occurred on this differentiated parent body.
How is the Bereba meteorite studied today?
Because it is linked to asteroid 4 Vesta, Bereba is studied to understand volcanic processes on planetary bodies. Specimens are also analyzed alongside data collected by NASA's Dawn spacecraft, which orbited Vesta.
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