meteorite

Possible iron-rich meteorite

Uncertain; likely an ordinary chondrite (stony meteorite), pending testing

AI-generated identification · may be incorrect

Dark brown-gray, weathered exterior with possible iron staining; typically weakly magnetic, dense, and nonvesicular. Ordinary chondrites have Mohs hardness about 6–7, metallic flecks, and a fine-grained silicate matrix; the photo alone cannot confirm these traits.

Identified August 13, 2026More meteorite →

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Physical properties

Formation & geological history

Formed from primitive Solar System materials about 4.56 billion years ago and survived atmospheric entry. Its rounded, dark fusion crust may indicate a meteorite, but terrestrial iron-rich rock or slag remains possible.

Uses & applications

Primarily a collectible or scientific specimen; confirmed meteorites can be valuable, while ordinary terrestrial rocks have little commercial use.

Geological facts

A true meteorite commonly shows a thin black fusion crust, regmaglypts, unusually high density, and magnetic response. Definitive identification requires a fresh cut, nickel/iron analysis, and preferably laboratory classification.

Field identification & locations

Test with a magnet and compare density; avoid destructive acid tests. Common meteorites include finds from Antarctica, deserts, and dry plains, but this specimen’s appearance is insufficient for authentication.