
mineral
Polished hematite bead (probable)
Hematite, Fe₂O₃
AI-generated identification · may be incorrectSmall polished gray-black sphere with metallic to submetallic luster; hematite hardness is about 5–6.5 Mohs, with no prominent cleavage and a relatively high specific gravity (~5.3). The image alone cannot exclude magnetite or an industrial metal bead.
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Physical properties
Small polished gray-black sphere with metallic to submetallic luster; hematite hardness is about 5–6.5 Mohs, with no prominent cleavage and a relatively high specific gravity (~5.3). The image alone cannot exclude magnetite or an industrial metal bead.
Formation & geological history
Hematite forms through oxidation in hydrothermal, sedimentary, and metamorphic environments, ranging from Precambrian deposits to modern weathering zones. Polishing and drilling indicate human processing.
Uses & applications
Used for jewelry beads, ornamental objects, pigment, and as an iron ore; it has little value as a tiny common bead. Typical value is about $1–$10, or $10–$30 if unusually fine or confirmed natural.
Geological facts
A diagnostic streak test gives hematite a reddish-brown streak, unlike magnetite’s black streak. Hematite is usually weakly magnetic or nonmagnetic, whereas magnetite is strongly magnetic.
Field identification & locations
Common sources include Brazil, Australia, South Africa, and the United States. Test with an unglazed ceramic tile for streak and a magnet; strong attraction suggests magnetite or another iron-rich material.
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