Rock Identifier
Polished black stone, likely hematite (Hematite (Fe₂O₃), possibly magnetite or a hematite-rich ironstone) — mineral
mineral

Polished black stone, likely hematite

Hematite (Fe₂O₃), possibly magnetite or a hematite-rich ironstone

AI-generated identification · may be incorrect

Dark gray to black, highly polished metallic-to-submetallic luster, with smooth rounded shaping. Hematite has Mohs hardness 5–6.5, specific gravity about 5.0–5.3, and no prominent cleavage; a red-brown streak is diagnostic. The image alone cannot reliably distinguish it from magnetite or black glass.

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Physical properties

Dark gray to black, highly polished metallic-to-submetallic luster, with smooth rounded shaping. Hematite has Mohs hardness 5–6.5, specific gravity about 5.0–5.3, and no prominent cleavage; a red-brown streak is diagnostic. The image alone cannot reliably distinguish it from magnetite or black glass.

Formation & geological history

Hematite forms through oxidation of iron-bearing minerals, hydrothermal activity, sedimentary chemical precipitation, and metamorphism; deposits range from Precambrian banded iron formations to younger ore bodies. This specimen appears tumbled or polished.

Uses & applications

Used extensively as iron ore, pigment, and ornamental material; polished pieces are sold as beads, cabochons, and pocket stones. Common specimens typically have modest value.

Geological facts

Despite its black appearance, hematite commonly produces a reddish-brown streak on unglazed porcelain. Magnetite is strongly magnetic, whereas hematite is usually weakly magnetic or nonmagnetic.

Field identification & locations

Common localities include Brazil, Australia, South Africa, the United States, and India. Test streak, magnetism, and density; a glassy black appearance with no streak could indicate obsidian or manufactured glass instead.