
sedimentary
Banded Iron Formation (Jasper-grade)
Banded Iron Formation (BIF) containing Hematite/Magnetite and Chert (SiO2)
Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown with creamy white or gray bands, Luster: Dull to sub-vitreous, Crystal structure: Microcrystalline/Cryptocrystalline, Specific Gravity: 2.6-3.3
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown with creamy white or gray bands, Luster: Dull to sub-vitreous, Crystal structure: Microcrystalline/Cryptocrystalline, Specific Gravity: 2.6-3.3
Formation & geological history
Formed in ancient marine environments between 2.4 and 1.8 billion years ago (Proterozoic Eon) through the precipitation of iron and silica during the Great Oxidation Event.
Uses & applications
Used primarily as iron ore for steel production; also used for lapidary work, jewelry, and as a collector's specimen.
Geological facts
These formations provide the primary evidence for the evolution of Earth's atmosphere and the introduction of free oxygen by early life forms like cyanobacteria.
Field identification & locations
Identify by the alternating thin layers (banding) of iron oxides and silica. Common in old shield regions like the Lake Superior area, Australia, and Brazil.
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