Rock Identifier
Pyrite-bearing dark metamorphic rock, likely schist or hornfels (Quartz–feldspar–mica matrix with pyrite (FeS₂); exact identification requires testing) — metamorphic
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 incorrect

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.

Identified More metamorphic
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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.