igneous
Meteorite (Chondrite)
Stony Meteorite (Ordinary Chondrite)
Hardness: 5-6 (Mohs). Color: Dark brown to black (fusion crust) or mottled grey/tan interior. Luster: Metallic to dull earthy. Physical features include the presence of chondrules (spherical mineral grains) and small metallic iron-nickel flecks. High specific gravity (very heavy for its size).
- Hardness
- 5-6 (Mohs)
- Luster
- Metallic to dull earthy
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Physical properties
Hardness: 5-6 (Mohs). Color: Dark brown to black (fusion crust) or mottled grey/tan interior. Luster: Metallic to dull earthy. Physical features include the presence of chondrules (spherical mineral grains) and small metallic iron-nickel flecks. High specific gravity (very heavy for its size).
Formation & geological history
Formed from molten droplets in the early solar nebula roughly 4.6 billion years ago. These extraterrestrial rocks originate from the asteroid belt and fall to Earth after surviving atmospheric entry.
Uses & applications
Vital for scientific research into the early solar system; ornamental use in jewelry; high demand among private mineral and astronomical collectors.
Geological facts
Chondrites are the most common type of meteorite falling to Earth, accounting for about 85% of falls. They contain tiny spheres called chondrules, which were once molten droplets in space and are among the oldest materials in the solar system.
Field identification & locations
Identify in the field by checking if the rock is attracted to a magnet (most chondrites are magnetic). Look for a thin, dark fusion crust and 'regmaglypts' (thumbprint-like indentations). Common locations for discovery include dry deserts (Sahara) and Antarctica where they are easily spotted against the ground.