
igneous
Chondrite Meteorite
Ordinary Chondrite (L or H group classification)
Hardness: 5-6 (Mohs), Color: Dark brown to black fusion crust with light gray or brownish interior, Luster: Metallic to dull, Crystal structure: Granular with visible chondrules, Specific gravity: 3.0 to 3.8
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Physical properties
Hardness: 5-6 (Mohs), Color: Dark brown to black fusion crust with light gray or brownish interior, Luster: Metallic to dull, Crystal structure: Granular with visible chondrules, Specific gravity: 3.0 to 3.8
Formation & geological history
Formed through the accretion of dust and granules in the early solar system approximately 4.5 billion years ago. These are remnants of protoplanetary disks that never underwent melting or differentiation.
Uses & applications
Scientific research into the origins of the solar system, private specimen collecting, and occasionally used in custom jewelry (slices).
Geological facts
Chondrites are the most common type of meteorite falling to Earth, accounting for about 86% of witnessed falls. They contain 'chondrules'—spherical grains that were once molten droplets in space.
Field identification & locations
Identify by checking for a fusion crust (thin burnt exterior), attraction to a strong magnet due to nickel-iron content, and a higher density than Earth rocks. Most common in desert environments where they are not easily eroded.