
metamorphic
Pyrite-bearing dark metamorphic rock, likely schist or hornfels
Quartz–feldspar–mica matrix with pyrite (FeS₂); exact identification requires testing
AI-generated identification · may be incorrectDark gray to black, fine-grained and weakly foliated, with brassy metallic pyrite flakes or crystals. Pyrite hardness is 6–6.5 Mohs and cubic crystals are common; the host rock appears harder than glass but has no obvious cleavage.
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Physical properties
Dark gray to black, fine-grained and weakly foliated, with brassy metallic pyrite flakes or crystals. Pyrite hardness is 6–6.5 Mohs and cubic crystals are common; the host rock appears harder than glass but has no obvious cleavage.
Formation & geological history
Likely formed when sulfur- and iron-bearing sediments or volcanic rocks were metamorphosed, allowing pyrite to crystallize; age cannot be determined from the image. Similar rocks occur in hydrothermal and contact-metamorphic zones.
Uses & applications
Primarily a collector specimen; pyrite may be mined for sulfur or historically for sulfuric-acid production, while the host rock has limited construction value. It is generally unsuitable for jewelry because pyrite tarnishes and can weather.
Geological facts
The brassy grains are most likely pyrite (“fool’s gold”), though chalcopyrite is a possible alternative. Pyrite commonly develops a dark oxidation coating and may produce sulfuric acid during weathering.
Field identification & locations
Check for a metallic luster, opaque brassy color, and a dark streak: pyrite streaks greenish-black, whereas gold streaks yellow. A steel-file test, streak plate, magnet test, and close inspection for cubic crystals can distinguish pyrite from other sulfides.
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