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Leoville

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description Leoville Overview

Leoville is a CV3 carbonaceous chondrite found in Kansas and assigned to the reduced subgroup of CV meteorites. It contains chondrules, calcium-aluminum-rich inclusions, metal, and fine-grained matrix that retain evidence of early Solar System processes. Its comparatively limited thermal and aqueous alteration makes Leoville particularly useful for laboratory studies of primitive nebular materials and chondrule formation.

help Leoville FAQ

What type of meteorite is the Leoville meteorite?

Leoville is classified as a CV3 carbonaceous chondrite, specifically belonging to the reduced (CVred) subgroup. This type of meteorite is incredibly rare and is known for containing some of the most primitive materials in the solar system.

Where was the Leoville meteorite found?

The meteorite was discovered near the town of Leoville in Kansas, USA. It was originally plowed up by a farmer working in a field, who kept it for years before its true extraterrestrial origin was identified by meteorite hunters.

Why is the Leoville meteorite scientifically important?

Leoville contains a wealth of chondrules and calcium-aluminum-rich inclusions (CAIs) that have remained largely unaltered since the birth of the Solar System. Scientists study these specific inclusions to learn about the exact age and formation processes of our early solar neighborhood.

Does the Leoville meteorite contain water or organic materials?

Like many carbonaceous chondrites, Leoville contains a fine-grained matrix that includes carbon and organic compounds. Its limited alteration on Earth makes it a valuable specimen for studying the prebiotic chemistry that preceded the origin of life.

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