Rock Identifier
Iron-rich rock fragment (likely hematite/goethite-rich ironstone) (Ironstone, composed chiefly of iron oxides/hydroxides such as hematite (Fe₂O₃) and goethite (FeO(OH)); exact identification requires testing) — sedimentary
sedimentary

Iron-rich rock fragment (likely hematite/goethite-rich ironstone)

Ironstone, composed chiefly of iron oxides/hydroxides such as hematite (Fe₂O₃) and goethite (FeO(OH)); exact identification requires testing

AI-generated identification · may be incorrect

Opaque, dark brown to rusty brown with earthy to subdued metallic luster; uneven fracture and no obvious crystal faces. Hardness and specific gravity cannot be reliably determined from the image; hematite is Mohs 5–6.5, goethite about 5–5.5.

Identified More sedimentary →
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Physical properties

Opaque, dark brown to rusty brown with earthy to subdued metallic luster; uneven fracture and no obvious crystal faces. Hardness and specific gravity cannot be reliably determined from the image; hematite is Mohs 5–6.5, goethite about 5–5.5.

Formation & geological history

Likely formed by iron-oxide accumulation and cementation in sediment, or by weathering of iron-bearing material. Ironstone forms in varied settings and ages; the specimen’s age and precise origin are unknown.

Uses & applications

Iron-rich material can be an iron ore when sufficiently concentrated; small fragments are mainly geological or educational collectibles, not typically used as gemstones.

Geological facts

Hematite leaves a reddish-brown streak, while goethite commonly gives a yellowish-brown streak—useful clues when identifying iron-rich specimens.

Field identification & locations

The rusty color and dense-looking, brown surface suggest ironstone, but appearance alone cannot distinguish it from other iron-rich rocks. Common in sedimentary deposits and weathered outcrops; a streak test and density measurement can help identify it.