igneous
Chondrite Meteorite
L or H type Ordinary Chondrite
Hardness: 5-6 (Mohs); Color: Dark brown to black (fusion crust) with gray/mottled interior; Luster: Sub-metallic to dull; Crystal structure: Contains rounded chondrules; Specific gravity: 3.0-3.8 (relatively heavy).
- Hardness
- 5-6 (Mohs)
- Luster
- Sub-metallic to dull
Identified More igneous →
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Physical properties
Hardness: 5-6 (Mohs); Color: Dark brown to black (fusion crust) with gray/mottled interior; Luster: Sub-metallic to dull; Crystal structure: Contains rounded chondrules; Specific gravity: 3.0-3.8 (relatively heavy).
Formation & geological history
Formed from the solar nebula over 4.5 billion years ago. These are primitive rocks that never underwent melting or differentiation in a planetary body.
Uses & applications
Scientific research into the origin of the solar system, private collecting, and occasionally used in high-end meteorite jewelry.
Geological facts
Chondrites are the most common type of meteorite falling to Earth, accounting for about 86% of all falls. They contain tiny spherical grains called chondrules, which were molten droplets in space before being accreted into asteroids.
Field identification & locations
Identify by looking for a dark fusion crust, presence of small metallic flakes (nickel-iron), attraction to a strong magnet, and a high weight relative to size. Found globally, especially in deserts like the Sahara or Antarctica.
