
mineral
Pyrite in Gossan
Iron Sulfide (FeS2) in Ferruginous Rock
Hardness: 6-6.5 (Pyrite), 5-6 (Gossan host); Color: Brass-yellow metallic grains in reddish-brown earthy matrix; Luster: Metallic (pyrite) to dull (matrix); Structure: Isometric crystals (cubic or pentagonal dodecahedron) or granular; Cleavage: Indistinct; Specific Gravity: Approx. 4.88-5.02.
- Hardness
- 6-6
- Color
- Brass-yellow metallic grains in reddish-brown earthy matrix
- Luster
- Metallic (pyrite) to dull (matrix)
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Physical properties
Hardness: 6-6.5 (Pyrite), 5-6 (Gossan host); Color: Brass-yellow metallic grains in reddish-brown earthy matrix; Luster: Metallic (pyrite) to dull (matrix); Structure: Isometric crystals (cubic or pentagonal dodecahedron) or granular; Cleavage: Indistinct; Specific Gravity: Approx. 4.88-5.02.
Formation & geological history
Formed through hydrothermal precipitation of iron sulfides in mineral veins, followed by surface weathering (oxidation) that creates the iron-rich 'gossan' capping. It can occur in deposits spanning various geological ages, often associated with Precambrian to Mesozoic volcanic activity.
Uses & applications
Pyrite is used as an ore of sulfur and for the production of sulfuric acid; in the past, it was used as a sparking material. The gossan is a classic 'iron hat' indicator used by geologists to locate deeper base-metal or gold deposits.
Geological facts
Pyrite is famously known as 'Fool\'s Gold' because its color often confused prospectors. Historically, gossans were vital to miners because they pointed to valuable copper, lead, or zinc ores lying beneath the oxidized surface layer.
Field identification & locations
Look for the characteristic brassy-yellow metallic glint against a rusty, porous, or earthy reddish-brown rock. It is commonly found in mining districts globally, particularly in Spain, Peru, and the Western USA. To identify pyrite, scratch it against a porcelain streak plate; it will leave a greenish-black streak, unlike real gold which leaves a yellow streak.
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