Rock Identifier
Iron-rich chondritic meteorite candidate (Unclassified stony meteorite; possible ordinary chondrite (H/L type)) — meteorite
meteorite

Iron-rich chondritic meteorite candidate

Unclassified stony meteorite; possible ordinary chondrite (H/L type)

AI-generated identification · may be incorrect

Dark gray-brown, irregular, partly weathered surface with rusty iron-oxide staining and possible metallic flecks; likely dense, nonvitreous, and weakly magnetic. Exact hardness, crystal structure, and specific gravity cannot be established from the image.

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Physical properties

Dark gray-brown, irregular, partly weathered surface with rusty iron-oxide staining and possible metallic flecks; likely dense, nonvitreous, and weakly magnetic. Exact hardness, crystal structure, and specific gravity cannot be established from the image.

Formation & geological history

Potential extraterrestrial rock formed from primitive solar-system material about 4.56 billion years ago, later altered by atmospheric entry and terrestrial weathering. Visual identification alone is insufficient; slag, basalt, or industrial iron-rich debris remain alternatives.

Uses & applications

Meteorites are valued mainly by collectors and researchers; scientifically confirmed ordinary chondrites commonly sell for about $1–$10 per gram, depending on authenticity, freshness, and classification.

Geological facts

A fusion crust, regmaglypts, high density, and magnetic response would support meteorite identification, but rusty weathering and a broken-looking surface are not diagnostic.

Field identification & locations

Check for a thin black fusion crust, unusually high density, and attraction to a magnet; avoid destructive tests and obtain nickel testing plus professional classification. Common finds occur in deserts, Antarctica, and dry agricultural regions.

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