
mineral
Bismuth
Bismuth (Bi)
AI-generated identification · may be incorrectHardness: 2.25 on Mohs scale; Color: Silver-white (native), Iridescent rainbow (lab-grown); Luster: Metallic; Crystal structure: Trigonal/Rhombohedral (Hopper crystals); Cleavage: Perfect; Specific gravity: 9.78
- Hardness
- 2
- Color
- Silver-white (native), Iridescent rainbow (lab-grown)
- Luster
- Metallic
Identified More mineral →
Explore Bismuth in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 2.25 on Mohs scale; Color: Silver-white (native), Iridescent rainbow (lab-grown); Luster: Metallic; Crystal structure: Trigonal/Rhombohedral (Hopper crystals); Cleavage: Perfect; Specific gravity: 9.78
Formation & geological history
Formed in hydrothermal veins and pegmatites. While it occurs naturally, specimens with this stair-step 'hopper' shape and rainbow color are lab-grown through a process of melting pure bismuth and allowing it to cool slowly so the edges grow faster than the centers.
Uses & applications
Used in metallurgy (low-melting alloys), cosmetics (bismuth oxychloride), pharmaceuticals (Pepto-Bismol), and as a lead substitute in shot and fishing sinkers. Highly popular as a decorative collectors' specimen.
Geological facts
Bismuth is one of the few substances (like water) that expands when it freezes. It is the most naturally diamagnetic element and has unusually low thermal conductivity. For a long time, it was thought to be stable, but it was discovered in 2003 to be slightly radioactive, though with a half-life a billion times longer than the age of the universe.
Field identification & locations
Identify in the field by its high density and silver-white color; however, the rainbow 'hopper' crystals shown are always man-made. Look for the distinct laboratory-perfect geometric 'steps' and brilliant iridescent oxidation caused by thin-film interference.
More like this
Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary