
mineral
Metallic sulfide-bearing rock, likely galena-rich ore
Galena (lead sulfide, PbS), possibly mixed with pyrite and host rock
AI-generated identification · may be incorrectSmall irregular gray specimen with metallic luster and granular/crystalline texture. Galena has Mohs hardness 2.5–2.75, very high specific gravity (~7.5), cubic crystals and perfect cubic cleavage; pyrite inclusions may be brassy and harder (6–6.5).
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Physical properties
Small irregular gray specimen with metallic luster and granular/crystalline texture. Galena has Mohs hardness 2.5–2.75, very high specific gravity (~7.5), cubic crystals and perfect cubic cleavage; pyrite inclusions may be brassy and harder (6–6.5).
Formation & geological history
Likely hydrothermal vein ore formed when hot, mineral-rich fluids deposited sulfides in fractures, commonly during the Paleozoic or younger. The image is insufficient to establish an exact species or age.
Uses & applications
Galena is the principal lead ore and historically supplied silver; specimens are collected but should not be used in jewelry or handled by children because lead dust is toxic.
Geological facts
Fresh galena is lead-gray and exceptionally heavy for its size; broken surfaces tarnish to dull gray. Pyrite can resemble gold but is much harder and commonly forms cubes.
Field identification & locations
Test cautiously by heft, streak, and cleavage: galena gives a dark gray streak and breaks into cubes, whereas pyrite gives a greenish-black streak and resists scratching. Common in Missouri, Idaho, Colorado, Peru, Australia, and Mexico.
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