meteorite
Chondrite Meteorite
Ordinary Chondrite (Undifferentiated Stony Meteorite)
Hardness: 5-6 (variable), Color: Dark brown to black fusion crust with a grayish-speckled interior, Luster: Metallic or dull, Structure: Contains small spherical grains called chondrules, Specific gravity: 3.0-3.8
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Physical properties
Hardness: 5-6 (variable), Color: Dark brown to black fusion crust with a grayish-speckled interior, Luster: Metallic or dull, Structure: Contains small spherical grains called chondrules, Specific gravity: 3.0-3.8
Formation & geological history
Formed roughly 4.6 billion years ago from the solar nebula; they are remnants of the early solar system that have not been modified by melting or differentiation of the parent body.
Uses & applications
Primarily used for scientific research to understand the origin of the solar system and as a highly sought-after collector's item.
Geological facts
Ordinary chondrites account for about 80% of all meteorites that fall to Earth. They are the oldest known materials on our planet, older than any terrestrial rock.
Field identification & locations
Identify by looking for a magnetic response, a thin dark 'fusion crust' from atmospheric entry, and a high density for its size. Often found in deserts or Antarctica where they stand out.
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