How to identify Native Silver
Ag
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Open the appTo correctly identify Native Silver (Ag), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Bright silver-white to silver-gray, often tarnishing to dull gray, black, or iridescent colors.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Bright metallic on fresh surfaces, duller on tarnished surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically found in dendritic (tree-like), wire-like, arborescent (branching), lamellar, or massive forms. Crystals are rare but can be cubic, octahedral, or dodecahedral.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Isometric system, commonly found as distorted crystals, wires, dendrites, or massive aggregates. Rarely forms distinct cubic or octahedral crystals.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. It exhibits a hackly fracture.
- 6
Geological Environment
The rock formation and setting where it occurs
Hydrothermal veins, often associated with sulfide minerals (e.g., argentite, galena, sphalerite), arsenides, and carbonates. Also found in the oxidized zones of silver-bearing ore deposits and occasionally in placer deposits.
Key Facts
- Hardness
- 2.5-3 on the Mohs scale
- Specific Gravity
- 10.4-10.5 (very heavy)
- Crystal System
- Isometric
- Color
- Silver-white, tarnishing to gray or black
- Luster
- Metallic
- Transparency
- Opaque
- Fracture
- Hackly
- Cleavage
- None
- Composition
- Elemental silver (Ag), often with minor amounts of gold (Au), copper (Cu), or mercury (Hg).
Physical characteristics
- Crystal Habit: Dendritic, wire-like, arborescent, massive, lamellar, rarely cubic or octahedral crystals.
- Cleavage Type: None
- Fracture Type: Hackly (jagged, sharp, and irregular, typical of malleable metals)
- Tenacity: Malleable and ductile
- Luster Type: Metallic
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