
mineral
Polished hematite (likely hematite-rich ironstone)
Hematite, Fe₂O₃; possibly mixed with magnetite or jasper
AI-generated identification · may be incorrectThe rounded polished specimen is dark gray to black with a metallic to submetallic reflective luster and reddish-brown edge tones. Hematite has Mohs hardness 5–6.5, trigonal crystal structure, no prominent cleavage, and specific gravity about 5.0–5.3; a red-brown streak is diagnostic.…
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Physical properties
The rounded polished specimen is dark gray to black with a metallic to submetallic reflective luster and reddish-brown edge tones. Hematite has Mohs hardness 5–6.5, trigonal crystal structure, no prominent cleavage, and specific gravity about 5.0–5.3; a red-brown streak is diagnostic. The rough material behind it appears granular and iron-rich.
Formation & geological history
Hematite forms through oxidation of iron-bearing minerals, hydrothermal activity, or chemical sedimentation, commonly in Precambrian banded iron formations and ironstone. The visible piece has been cut and tumbled/polished, so its precise age and source cannot be determined.
Uses & applications
Used as an iron ore, pigment, polishing medium, and ornamental stone. Polished hematite is common in inexpensive jewelry and worry stones.
Geological facts
A strong red-to-reddish-brown streak on unglazed porcelain distinguishes hematite from similarly shiny magnetite. It is weakly to nonmagnetic, whereas magnetite is strongly magnetic.
Field identification & locations
Likely identification: polished hematite or hematite-rich ironstone. Test the streak and magnetism; hematite commonly occurs in iron-rich rocks worldwide, including California, though the image alone cannot establish a local source near 38.7°N, 121.3°W.
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