
mineral
Weathered metallic-looking rock, possibly hematite-bearing ironstone
Hematite-rich ironstone; hematite Fe₂O₃, potentially with magnetite Fe₃O₄ and quartz
AI-generated identification · may be incorrectHardness about 5–6.5 Mohs; dark gray to brown with metallic or submetallic luster and iridescent surface tarnish. Typically massive rather than visibly crystalline, with a reddish-brown streak; specific gravity commonly 4.5–5.3.
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Physical properties
Hardness about 5–6.5 Mohs; dark gray to brown with metallic or submetallic luster and iridescent surface tarnish. Typically massive rather than visibly crystalline, with a reddish-brown streak; specific gravity commonly 4.5–5.3.
Formation & geological history
Likely formed through oxidation or concentration of iron minerals in hydrothermal, sedimentary, or weathering environments; age cannot be determined from the photograph. The polished-looking sheen may result from natural weathering or surface abrasion.
Uses & applications
Used as an iron ore and pigment; attractive pieces are collected as mineral specimens. It is generally unsuitable for gemstone jewelry unless cut and polished.
Geological facts
Hematite’s diagnostic streak is red to reddish brown even when the specimen appears black or metallic. The image alone cannot distinguish hematite from magnetite, weathered ironstone, or an iron-rich meteorite.
Field identification & locations
Check the streak on unglazed porcelain, test magnetism, and inspect for metallic density; hematite is usually weakly magnetic or nonmagnetic, whereas magnetite is strongly magnetic. Common sources include Brazil, Australia, the United States, and India.
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