
sedimentary
Limonite-stained Gossan/Ironstone
Goethite and Hematite (Fe2O3 • nH2O)
Hardness: 4-5.5 (variable); Color: Dark brown to metallic gray with yellowish-orange oxidation; Luster: Sub-metallic to dull; Structure: Masses or crusts; Cleavage: None
- Hardness
- 4-5
- Color
- Dark brown to metallic gray with yellowish-orange oxidation
- Luster
- Sub-metallic to dull
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Physical properties
Hardness: 4-5.5 (variable); Color: Dark brown to metallic gray with yellowish-orange oxidation; Luster: Sub-metallic to dull; Structure: Masses or crusts; Cleavage: None
Formation & geological history
Formed through the intensive chemical weathering and oxidation of iron-rich sulfide minerals or other iron-bearing rocks, often indicating a subsurface ore deposit.
Uses & applications
Historically used as a low-grade iron ore; currently used as a geological indicator for prospecting metal deposits and as a source of pigments (ochre).
Geological facts
Gossans are known as 'iron hats' to miners because they sit over the top of unoxidized ore bodies and were used since antiquity to find copper, gold, and silver.
Field identification & locations
Identifiable by its heavy weight relative to surrounding rocks and its distinct rusty-yellow or orange-brown staining. Found in mining districts and areas with high metal sulfide mineralization.
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