
meteorite
Chondrite Meteorite
Stony Meteorite (Ordinary Chondrite)
Hardness: 5-6 (Mohs); Color: dark brown to black fusion crust with gray interior; Luster: matte to sub-metallic; Structure: contains small spherical grains called chondrules; Specific Gravity: 3.0-3.8
- Hardness
- 5-6 (Mohs)
- Color
- dark brown to black fusion crust with gray interior
- Luster
- matte to sub-metallic
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Physical properties
Hardness: 5-6 (Mohs); Color: dark brown to black fusion crust with gray interior; Luster: matte to sub-metallic; Structure: contains small spherical grains called chondrules; Specific Gravity: 3.0-3.8
Formation & geological history
Formed in the early solar system approximately 4.5 billion years ago from the solar nebula. These are fragments of asteroids that have fallen to Earth, characterized by a fusion crust formed during atmospheric entry.
Uses & applications
Extremely high value for scientific research into the origins of the solar system; highly prized by private collectors and used in custom jewelry.
Geological facts
Chondrites are the most common type of meteorite falling to Earth, representing about 86% of witnessed falls. They contain the oldest solid materials in our solar system.
Field identification & locations
Identify by the presence of a thin, dark fusion crust, magnetic attraction due to nickel-iron grains, and a high density compared to terrestrial rocks. Commonly found in deserts or Antarctica.
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