Rock Identifier
Polished magnetite-rich ironstone (probable magnetite/hematite nodule) (Magnetite, Fe₃O₄, possibly mixed with hematite, Fe₂O₃, and iron-bearing gangue) — mineral
mineral

Polished magnetite-rich ironstone (probable magnetite/hematite nodule)

Magnetite, Fe₃O₄, possibly mixed with hematite, Fe₂O₃, and iron-bearing gangue

AI-generated identification · may be incorrect

Dark steel-gray to black, metallic-to-submetallic luster, unevenly polished surface, opaque, and likely strongly magnetic; magnetite hardness 5.5–6.5 Mohs, cubic crystal structure, no cleavage, specific gravity about 5.2. Exact identification requires a magnet and streak test.

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Physical properties

Dark steel-gray to black, metallic-to-submetallic luster, unevenly polished surface, opaque, and likely strongly magnetic; magnetite hardness 5.5–6.5 Mohs, cubic crystal structure, no cleavage, specific gravity about 5.2. Exact identification requires a magnet and streak test.

Formation & geological history

Likely formed by oxidation, hydrothermal alteration, or concentration of iron minerals in a volcanic or metamorphic host; age cannot be determined from the photograph. Rounded shape may reflect natural weathering or human polishing.

Uses & applications

Used historically as iron ore and pigment source; attractive polished pieces are sold as mineral specimens or curiosities, but this example is not suitable for jewelry without secure mounting.

Geological facts

Magnetite is naturally magnetic and can produce lodestone. Hematite-rich material commonly develops reddish-brown streak despite its black appearance.

Field identification & locations

Test with a strong magnet, inspect the streak on unglazed porcelain, and compare density; magnetite gives a black streak, while hematite gives red-brown. Common localities include Sweden, Russia, South Africa, the United States, and Mexico.