Mineral

Chondrite Meteorite

Ordinary Chondrite (L or H Type)

AI-generated identification · may be incorrect

Hardness: 5-6 (variable based on metallic content); Color: Mottled brown, orange, and gray due to oxidation; Luster: Sub-metallic to dull; Crystal structure: Contains spherical chondrules; Specific gravity: 3.0 to 3.8

Hardness: 5-6 (variable based on metallic content)
Color: Mottled brown, orange, and gray due to oxidation
Luster: Sub-metallic to dull

Identified April 8, 2026More mineral →

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Physical properties

Formation & geological history

Formed in the early solar system roughly 4.5 billion years ago from solar nebula dust and grains. Found as terrestrial falls typically in arid desert regions or Antarctica.

Uses & applications

Primarily used for scientific research, education, and private collection. Can be used in 'out of this world' jewelry when sliced and polished.

Geological facts

Chondrites are the most common type of meteorite falling to Earth, accounting for about 86% of all falls. They contain the oldest solid materials in our solar system.

Field identification & locations

Identify by looking for a fusion crust (exterior), magnetic attraction (due to iron-nickel flakes), and the presence of tiny spherical chondrules inside when cut.