Rock Identifier
Tumbled hematite (Hematite (Fe₂O₃), likely specular or massive hematite) — mineral
mineral

Tumbled hematite

Hematite (Fe₂O₃), likely specular or massive hematite

AI-generated identification · may be incorrect

Dark gray to black, metallic-to-submetallic luster, smooth tumbled surface, and opaque appearance; Mohs hardness 5–6.5, trigonal crystal system, specific gravity about 5.3, with no obvious cleavage.

Identified More mineral
Explore Tumbled hematite in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Dark gray to black, metallic-to-submetallic luster, smooth tumbled surface, and opaque appearance; Mohs hardness 5–6.5, trigonal crystal system, specific gravity about 5.3, with no obvious cleavage.

Formation & geological history

Forms through oxidation of iron-rich fluids, sedimentary iron formations, hydrothermal veins, or weathering zones; specimens may range from Precambrian deposits to much younger surface concentrations.

Uses & applications

Used as an iron ore, pigment, polishing abrasive, and ornamental or metaphysical stone; attractive polished pieces are collected and sometimes made into jewelry.

Geological facts

Hematite commonly leaves a distinctive red to reddish-brown streak even when its surface is black or metallic. Its high density makes it feel unusually heavy for its size.

Field identification & locations

Common in Brazil, Australia, China, the United States, Canada, and South Africa. Confirm with a streak test on unglazed porcelain: hematite produces a red-brown streak, unlike magnetite, which produces a black streak and is strongly magnetic.