Rock Identifier
Polished hematite-rich ironstone (Hematite (Fe₂O₃), likely in a magnetite/goethite-bearing ironstone matrix) — mineral
mineral

Polished hematite-rich ironstone

Hematite (Fe₂O₃), likely in a magnetite/goethite-bearing ironstone matrix

AI-generated identification · may be incorrect

Hardness about 5–6.5 Mohs; black to reddish-brown, metallic to submetallic luster, opaque, with a smooth polished surface. Hematite commonly has a red-brown streak and specific gravity around 5.0–5.3; magnetite-bearing material may be magnetic.

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Physical properties

Hardness about 5–6.5 Mohs; black to reddish-brown, metallic to submetallic luster, opaque, with a smooth polished surface. Hematite commonly has a red-brown streak and specific gravity around 5.0–5.3; magnetite-bearing material may be magnetic.

Formation & geological history

Formed by chemical precipitation, oxidation, or metamorphism of iron-rich sediments and hydrothermal deposits, commonly Precambrian in age. The specimen appears tumbled or polished rather than naturally weathered.

Uses & applications

Used as an iron ore, pigment, abrasive, and ornamental stone; polished pieces are sold for jewelry and collecting. It is generally more decorative than gem-grade.

Geological facts

Hematite’s name derives from the Greek word for blood, referencing its red streak or powder. Its dark metallic appearance can resemble magnetite, but a streak test and magnet check help distinguish them.

Field identification & locations

Common in banded iron formations and iron-rich deposits worldwide, especially Brazil, Australia, India, and the Lake Superior region. Test an inconspicuous area for a reddish streak; magnetism suggests magnetite or mixed iron oxides.