igneous
Chondrite Meteorite
Stony Meteorite (L, H, or LL Chondrite)
Hardness: 4.5-5.5 Mohs (variable); Color: Dark brown to black (fusion crust) or grey interior; Luster: Dull/Sub-metallic; Crystal structure: Amorphous groundmass with visible chondrules; Specific Gravity: 3.0-3.8; Weakly magnetic.
- Hardness
- 4
- Color
- Dark brown to black (fusion crust) or grey interior
- Luster
- Dull/Sub-metallic
Identified More igneous →
Explore Chondrite Meteorite in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 4.5-5.5 Mohs (variable); Color: Dark brown to black (fusion crust) or grey interior; Luster: Dull/Sub-metallic; Crystal structure: Amorphous groundmass with visible chondrules; Specific Gravity: 3.0-3.8; Weakly magnetic.
Formation & geological history
Formed through the accretion of dust and grains in the early solar nebula approximately 4.56 billion years ago. These are fragments of asteroids that fall to Earth through the atmosphere.
Uses & applications
Primary use is scientific research into the early solar system; ornamental use in jewelry; high demand among private collectors and museums.
Geological facts
Chondrites represent the oldest solid material in the solar system. They contain 'chondrules'—small, spherical grains that were once molten droplets in space before the planets formed.
Field identification & locations
Identify in the field by checking for a thin, dark 'fusion crust' from atmospheric entry, a attracted to magnets, and often higher density than local terrestrial rocks. Commonly found in deserts or Antarctica.
