
mineral
Hematite Pebble
Hematite (Fe2O3)
Hardness: 5.5-6.5 on Mohs scale. Color: Dark gray to black, often with a metallic sheen or reddish undertones. Luster: Metallic to submetallic or earthy. Crystal system: Trigonal. Streak: Cherry-red to reddish-brown. Specific gravity: 5.26.
- Hardness
- 5
- Luster
- Metallic to submetallic or earthy
- Streak
- Cherry-red to reddish-brown
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Physical properties
Hardness: 5.5-6.5 on Mohs scale. Color: Dark gray to black, often with a metallic sheen or reddish undertones. Luster: Metallic to submetallic or earthy. Crystal system: Trigonal. Streak: Cherry-red to reddish-brown. Specific gravity: 5.26.
Formation & geological history
Forms in diverse environments including hydrothermal veins, sedimentary iron formations (BIFs), and volcanic regions. Formed over billions of years through the precipitation of iron-rich minerals in ancient oceans.
Uses & applications
Used as an ore of iron, in jewelry, carvings, and as a polishing powder (jeweler's rouge). Also collected as a mineral specimen.
Geological facts
Hematite is the primary ore of iron. When finely powdered, it produces a distinct reddish-brown streak, which is a key diagnostic property despite the stone's dark, metallic appearance.
Field identification & locations
Easily identified by its characteristic heavy weight relative to its size (high specific gravity), dark metallic appearance, and unmistakable reddish-brown streak when scratched on unglazed porcelain. Commonly found in stream beds as smoothed pebbles or in massive deposits worldwide.
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