igneous
Chondrite Meteorite
Ordinary Chondrite (L or H type)
Hardness: 5-6 Mohs. Color: Dark brown to black fusion crust with grey/brown interior. Luster: Dull to sub-metallic. Structure: Granular with visible chondrules. Specific gravity: 3.0-3.8 g/cm3.
- Hardness
- 5-6 Mohs
- Color
- Dark brown to black fusion crust with grey/brown interior
- Luster
- Dull to sub-metallic
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Physical properties
Hardness: 5-6 Mohs. Color: Dark brown to black fusion crust with grey/brown interior. Luster: Dull to sub-metallic. Structure: Granular with visible chondrules. Specific gravity: 3.0-3.8 g/cm3.
Formation & geological history
Formed from dust and grains in the early solar system roughly 4.5 billion years ago. These are undifferentiated rocks from asteroids that never underwent melting.
Uses & applications
Highly valued for scientific research into the early solar system, private collections, and occasionally used in unique jewelry or watch faces.
Geological facts
Chondrites are the most common type of meteorite falling to Earth, accounting for about 86% of all witnessed falls. They contain small round grains called chondrules.
Field identification & locations
Identify by a dark, thin fusion crust, magnetic attraction due to iron-nickel content, and high density compared to terrestrial rocks. Commonly found in deserts like the Sahara or Antarctica.
