How to identify Native Bismuth
Bismuth
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Open the appTo correctly identify Native Bismuth (Bismuth), 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
Silvery-white with a distinct reddish or pinkish tinge, often tarnishing to iridescent yellow, blue, or purple.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Metallic, bright.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically massive, granular, or lamellar. Crystals are rare in nature, but when found, they are often tabular or acicular.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Trigonal system. Natural crystals are rare, often anhedral, granular, or lamellar. Synthetic crystals exhibit distinctive hopper growth.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Perfect basal cleavage on {0001}.
- 6
Geological Environment
The rock formation and setting where it occurs
Hydrothermal veins, pegmatites, and contact metamorphic deposits, often associated with tin, tungsten, silver, cobalt, nickel, and uranium ores.
Key Facts
- Hardness
- 2-2.5 on the Mohs scale.
- Specific Gravity
- 9.78 g/cm³ (very dense).
- Crystal System
- Trigonal (hexagonal-rhombohedral).
- Color
- Silvery-white with a reddish or pinkish tinge, often tarnishing to iridescent yellow, blue, or purple.
- Luster
- Metallic.
- Transparency
- Opaque.
- Fracture
- Uneven to subconchoidal.
- Cleavage
- Perfect basal cleavage on {0001}.
- Composition
- Elemental Bismuth (Bi).
Physical characteristics
- Crystal Habit: Massive, granular, lamellar, arborescent, reticulated. Natural crystals are rare, typically tabular or acicular. Synthetic crystals are often hopper-shaped and iridescent.
- Cleavage Type: Perfect basal cleavage on {0001}.
- Fracture Type: Uneven to subconchoidal.
- Tenacity: Brittle.
- Luster Type: Metallic.
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