Rock Identifier
Tumbled hematite (specular iron ore) (Hematite, α-Fe₂O₃) — mineral
mineral

Tumbled hematite (specular iron ore)

Hematite, α-Fe₂O₃

AI-generated identification · may be incorrect

Dark steel-gray to black, metallic-to-submetallic luster; hardness 5–6.5 Mohs, trigonal crystal structure, no prominent cleavage, and specific gravity about 5.0–5.3. The rounded shape and shine indicate polishing; visual identification is not definitive.

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Physical properties

Dark steel-gray to black, metallic-to-submetallic luster; hardness 5–6.5 Mohs, trigonal crystal structure, no prominent cleavage, and specific gravity about 5.0–5.3. The rounded shape and shine indicate polishing; visual identification is not definitive.

Formation & geological history

Forms through oxidation and precipitation of iron, in sedimentary iron formations, hydrothermal veins, and weathered iron-rich rocks. Hematite occurs from ancient Precambrian deposits to modern environments.

Uses & applications

Used as iron ore and pigment; polished pieces are sold as inexpensive collectibles and jewelry stones.

Geological facts

Despite its metallic appearance, hematite is an iron oxide; its streak is characteristically reddish brown.

Field identification & locations

Common worldwide, including major deposits in Australia, Brazil, and the Lake Superior region. A reddish-brown streak on unglazed porcelain helps distinguish it from lookalikes.