Rock Identifier
Chondrite Meteorite (Ordinary Chondrite (L or H group classification)) — igneous
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

Identified More igneous
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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.