Rock Identifier
Specular hematite (iron ore), possibly with goethite (Hematite, Fe₂O₃; the metallic gray material may include goethite, FeO(OH), and other iron oxides) — mineral
mineral

Specular hematite (iron ore), possibly with goethite

Hematite, Fe₂O₃; the metallic gray material may include goethite, FeO(OH), and other iron oxides

AI-generated identification · may be incorrect

Dark steel-gray to black, strongly metallic to submetallic luster, irregular massive/botryoidal texture, and reddish-brown internal streaks. Hardness about 5–6.5 Mohs; specific gravity roughly 4.9–5.3; no prominent cleavage. The shiny surface may be natural specular hematite or partly polished/coated.

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Physical properties

Dark steel-gray to black, strongly metallic to submetallic luster, irregular massive/botryoidal texture, and reddish-brown internal streaks. Hardness about 5–6.5 Mohs; specific gravity roughly 4.9–5.3; no prominent cleavage. The shiny surface may be natural specular hematite or partly polished/coated.

Formation & geological history

Forms through oxidation and hydrothermal alteration of iron-rich rocks, commonly in banded iron formations, veins, and weathering zones. Hematite deposits range from Precambrian to recent, with age impossible to determine from the photograph.

Uses & applications

Used extensively as iron ore and pigment; attractive polished pieces are sold as hematite specimens and inexpensive jewelry. This small irregular specimen has modest commercial value.

Geological facts

Hematite produces a distinctive red to reddish-brown streak even when its surface is black and metallic. Its high density and magnetism—usually weak, though associated magnetite can be strongly magnetic—help distinguish it from slag.

Field identification & locations

Common localities include Brazil, Australia, South Africa, the Lake Superior region, and England. Test an inconspicuous area with an unglazed tile for red streak; check density and magnetism, since visual identification alone cannot exclude industrial slag.