Rock Identifier
Iron-rich quartzite or ironstone (Ferruginous quartzite, likely quartz (SiO₂) with hematite/goethite (Fe₂O₃/FeO(OH))) — metamorphic
metamorphic

Iron-rich quartzite or ironstone

Ferruginous quartzite, likely quartz (SiO₂) with hematite/goethite (Fe₂O₃/FeO(OH))

AI-generated identification · may be incorrect

Hardness approximately 6–7 (quartz-rich areas), with rusty red-brown, yellow-brown, and gray coloration; generally dull to granular, with local earthy or weakly metallic iron-oxide luster. Massive, fine- to medium-grained texture; no obvious cleavage, and high specific gravity where iron-rich.

Identified More metamorphic
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Physical properties

Hardness approximately 6–7 (quartz-rich areas), with rusty red-brown, yellow-brown, and gray coloration; generally dull to granular, with local earthy or weakly metallic iron-oxide luster. Massive, fine- to medium-grained texture; no obvious cleavage, and high specific gravity where iron-rich.

Formation & geological history

Likely formed when quartz-rich sediment was metamorphosed and impregnated or cemented by iron oxides; oxidation commonly produces the rust-colored surface. Exact geological age and locality cannot be determined from the photograph alone.

Uses & applications

Primarily a collector specimen or educational sample; iron-rich varieties may be considered low-grade iron ore, but this piece is unlikely to have commercial value without assay.

Geological facts

The reddish-brown colors commonly come from hematite, while yellow-orange coatings often indicate goethite or limonite. A streak test and magnet test can help distinguish iron-rich rock from ordinary quartzite.

Field identification & locations

Common in banded-iron formations, weathered iron deposits, and metamorphic terrains worldwide. Test an inconspicuous area: quartz scratches glass, hematite leaves a red-brown streak, and magnetite causes a strong magnet response.