Rock Identifier
Likely polished hematite (Hematite, α-Fe₂O₃ (identification is tentative from the photo)) — mineral
mineral

Likely polished hematite

Hematite, α-Fe₂O₃ (identification is tentative from the photo)

AI-generated identification · may be incorrect

Small, polished, dark gray-to-brown piece with a reflective surface. Hematite has Mohs hardness 5–6.5, a trigonal crystal structure, and a distinctive reddish-brown streak; the image alone cannot confirm these traits.

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Physical properties

Small, polished, dark gray-to-brown piece with a reflective surface. Hematite has Mohs hardness 5–6.5, a trigonal crystal structure, and a distinctive reddish-brown streak; the image alone cannot confirm these traits.

Formation & geological history

Hematite forms in many settings, including iron-rich sediments, hydrothermal veins, and weathered iron deposits; specimens range from Precambrian to recent. The pictured piece appears shaped and polished from natural material.

Uses & applications

Commonly used as an iron ore and fashioned into beads, carvings, and decorative objects.

Geological facts

Despite its metallic appearance, hematite is not magnetic in its common form and typically leaves a red-brown streak.

Field identification & locations

Check for a reddish-brown streak on unglazed porcelain and a relatively high heft; dark polished stones can resemble other minerals. Hematite occurs worldwide, including Brazil, Australia, and the Lake Superior region.