Rock Identifier
Native metallic specimen, possibly galena or a sulfide-rich ore fragment (Tentatively galena (lead sulfide, PbS), possibly mixed with iron/copper sulfides) — mineral
mineral

Native metallic specimen, possibly galena or a sulfide-rich ore fragment

Tentatively galena (lead sulfide, PbS), possibly mixed with iron/copper sulfides

AI-generated identification · may be incorrect

Small dark gray-to-silver metallic mass with uneven granular surfaces and apparent oxidation. Galena has Mohs hardness 2.5–3, cubic cleavage, metallic luster, and high specific gravity (~7.5); exact properties cannot be confirmed from the image.

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Physical properties

Small dark gray-to-silver metallic mass with uneven granular surfaces and apparent oxidation. Galena has Mohs hardness 2.5–3, cubic cleavage, metallic luster, and high specific gravity (~7.5); exact properties cannot be confirmed from the image.

Formation & geological history

Likely formed in hydrothermal ore veins as sulfide minerals precipitated from hot, mineral-rich fluids, commonly during the Paleozoic–Mesozoic or younger. The brown coating may represent weathering products such as iron oxides.

Uses & applications

Galena is an important historical source of lead and silver; attractive crystals are collector specimens, but lead-bearing pieces should not be handled extensively or used near food.

Geological facts

Its unusually heavy feel, bright metallic gray color, and cubic cleavage are characteristic of galena. Avoid sanding, breaking, or ingesting dust, and wash hands after handling.

Field identification & locations

Test cautiously for high density and cubic cleavage; a streak test on unglazed porcelain is dark gray, but do not perform it indoors because of toxic dust. Common localities include Missouri, Idaho, Mexico, Peru, and Australia.