Rock Identifier
Weathered iron-rich rock, possibly basalt or ironstone (Likely vesicular basalt or ferruginous breccia; exact identification requires testing) — igneous
igneous

Weathered iron-rich rock, possibly basalt or ironstone

Likely vesicular basalt or ferruginous breccia; exact identification requires testing

AI-generated identification · may be incorrect

Dark brown-black, strongly weathered, dull to slightly metallic luster with rusty orange iron-oxide patches and fractures. Estimated hardness 5–6 if basalt; magnetism and specific gravity would help distinguish ironstone or meteorite; crystal structure is fine-grained and cleavage is absent.

Identified More igneous
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Physical properties

Dark brown-black, strongly weathered, dull to slightly metallic luster with rusty orange iron-oxide patches and fractures. Estimated hardness 5–6 if basalt; magnetism and specific gravity would help distinguish ironstone or meteorite; crystal structure is fine-grained and cleavage is absent.

Formation & geological history

Probably an terrestrial volcanic or iron-rich rock altered by oxidation and weathering over geological time. The rusty coloration reflects conversion of iron-bearing minerals to limonite/goethite.

Uses & applications

Common material has little commercial value, though basalt is used for aggregate and construction; attractive pieces may be collected as field specimens.

Geological facts

Its irregular shape, earthy weathering, and orange oxidation are more typical of terrestrial rock than a meteorite. A strong magnet, visible vesicles, and a streak test are useful checks.

Field identification & locations

Common in volcanic or iron-rich terrains worldwide. Test with a magnet, inspect for bubbles or metallic grains, and perform a streak test on unglazed ceramic; a meteorite typically has a dense interior and fusion crust, not porous rusty surfaces.