Rock Identifier
Native silver (likely) (Silver, Ag; possibly silver-bearing sulfide or mica contamination) — mineral
mineral

Native silver (likely)

Silver, Ag; possibly silver-bearing sulfide or mica contamination

AI-generated identification · may be incorrect

Bright silvery-white, metallic luster, irregular leafy or wiry masses, and apparent malleability. Native silver has Mohs hardness 2.5–3, cubic crystal structure, no cleavage, and high specific gravity (~10.5); the image alone cannot confirm composition.

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Physical properties

Bright silvery-white, metallic luster, irregular leafy or wiry masses, and apparent malleability. Native silver has Mohs hardness 2.5–3, cubic crystal structure, no cleavage, and high specific gravity (~10.5); the image alone cannot confirm composition.

Formation & geological history

Forms hydrothermally in veins and cavities, commonly with quartz, calcite, galena, and other sulfides, through precipitation from metal-rich fluids. Deposits are generally associated with volcanic or metamorphic terrains of varied ages.

Uses & applications

Used historically for coinage, jewelry, electrical contacts, photography, solder, and industrial catalysts; attractive crystallized specimens have collector value.

Geological facts

Native silver commonly develops thin sheets, wires, dendritic growths, and twisted “leaf” forms. It tarnishes to gray or black sulfides and is easily scratched or bent compared with most metallic minerals.

Field identification & locations

Confirm with a streak test (silvery-gray), density, malleability, and ideally conductivity or laboratory analysis; avoid acid or destructive tests. Common localities include Mexico, Peru, Germany, Canada, and the United States, especially Michigan and Colorado.