
metamorphic
Iron-rich metamorphic rock, likely magnetite–hematite-bearing ironstone
Banded or massive iron formation (BIF), chiefly hematite (Fe₂O₃) and magnetite (Fe₃O₄), with quartz and possible iron silicates
AI-generated identification · may be incorrectDark reddish-brown to black, earthy-to-submetallic luster, granular texture, and irregular fracture; hardness about 5–6.5, with magnetite-bearing pieces strongly magnetic and high specific gravity (~4.5–5.3).
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Physical properties
Dark reddish-brown to black, earthy-to-submetallic luster, granular texture, and irregular fracture; hardness about 5–6.5, with magnetite-bearing pieces strongly magnetic and high specific gravity (~4.5–5.3).
Formation & geological history
Formed when iron minerals and silica precipitated from ancient oxygen-poor oceans, later compacted, metamorphosed, and locally oxidized; many deposits are Precambrian, roughly 2.5–1.8 billion years old.
Uses & applications
Major source of iron ore for steelmaking; attractive dense specimens are collected, while polished hematite-rich material is occasionally used ornamentally.
Geological facts
The specimen’s rough, rusty appearance is consistent with iron oxidation, but an image cannot confirm whether it is BIF, hematite-rich ore, or magnetite-rich skarn.
Field identification & locations
Look for red-brown streak (hematite) or black streak and magnetism (magnetite); common in the Lake Superior region, Australia, Brazil, India, and South Africa. A streak test and magnet are useful field checks.
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