igneous
Chondrite Meteorite
Ordinary Chondrite (L or H group)
Hardness: 5-6 Mohs. Color: Dark grey to brown exterior (fusion crust), grey interior with metallic flakes. Luster: Metallic flecks within a dull stony matrix. Structure: Contains chondrules (round grains) and nickel-iron grains. Specific Gravity: 3.0-3.8.
- Hardness
- 5-6 Mohs
- Luster
- Metallic flecks within a dull stony matrix
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: 5-6 Mohs. Color: Dark grey to brown exterior (fusion crust), grey interior with metallic flakes. Luster: Metallic flecks within a dull stony matrix. Structure: Contains chondrules (round grains) and nickel-iron grains. Specific Gravity: 3.0-3.8.
Formation & geological history
Formed from the solar nebula approximately 4.5 billion years ago. These are primitive rocks that never underwent melting or differentiation within a planetary body.
Uses & applications
Scientific research into the origin of the solar system, private collection, and occasionally used in custom jewelry or decorative watches.
Geological facts
Chondrites are the most common type of meteorite falling to Earth, accounting for about 85% of all falls. They contain the oldest solid materials in the solar system.
Field identification & locations
Identify by the presence of a thin, dark fusion crust on the exterior and small, shiny metal flakes on a cut surface. Usually magnetic. Commonly found in deserts or Antarctica where they are easily spotted.
