meteorite

L-Chondrite Meteorite Fragment

Stony Meteorite (Ordinary Chondrite, L-type)

AI-generated identification · may be incorrect

Hardness: 5-6 (variable), Color: Dark brown to black Fusion Crust with reddish oxidation, Luster: Dull/Metallic, Structure: Fragmented with visible chondrules potentially inside, Specific Gravity: 3.0-3.5

Identified July 20, 2026More meteorite →

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Physical properties

Formation & geological history

Formed in the early solar system approximately 4.5 billion years ago. These are fragments from asteroids that fell through Earth's atmosphere, developing a fusion crust due to atmospheric friction.

Uses & applications

Scientific research, education, and high-value private collecting.

Geological facts

Ordinary chondrites make up about 85% of all meteorite falls. The 'L' stands for 'Low iron' content compared to H-chondrites. They are essentially 'time capsules' from the birth of our solar system.

Field identification & locations

Identified by its distinctive dark fusion crust and magnetic properties. Look for a 'rust' colored oxidation where the interior is exposed. Found globally, often in deserts or ice fields where they contrast with the ground.