Bismuthinite

Bi2S3
IMA status
  • Approved
  • Grandfathered
IMA symbol
Bin
Discovered
1832
Also known as
  • Bismuth Glance
  • Bismuthine
  • Bismutholamprite
  • +2 more

History

The mineral's name is simply its recipe read aloud. Bismuthinite is bismuth sulfide — bismuth bonded to sulfur — and it was named for that composition. The metal itself lent the name, and the metal's own story is older and stranger than the mineral's.

For centuries, no one was sure bismuth was its own thing. Early on it was confused with tin and lead, which it resembles. The first written hint that it stood apart came in 1546. The German scholar Georgius Agricola described it as a distinct metal, in a family that also held tin and lead. The word bismuth traces back to this period too — a neo-Latin form, bisemutum, derived from the German Wismut, perhaps from weiße Masse, meaning "white mass".

Certainty took two more centuries. Johann Heinrich Pott began clearing up the confusion in 1738, and in 1753 Claude François Geoffroy showed that bismuth is distinct from lead and tin. Only after the metal was pinned down could its ores be named for it.

That naming came in 1832, when the French mineralogist François Sulpice Beudant called the sulfide bismuthine. The mineral was first reported the same year, from the silver mines of Potosí in Bolivia.

Industrial & practical applications

Bismuthinite earns its keep underground, not on the shelf. It is mined as an ore — a rock worth digging for the metal locked inside it — and that metal is bismuth. Everything people actually handle is made from the refined metal, not the raw mineral. So the uses below belong to smelted bismuth and its compounds, drawn from this ore and others.

Most bismuth never starts as bismuthinite at all. The metal is mostly produced by refining, as a byproduct of extracting lead, copper, tin, molybdenum, and tungsten. The ore is one feedstock among several for the smelter.

The refined metal's standout trick is melting at low temperatures. Bismuth goes into low-melting alloys, also called fusible alloys, that turn liquid in hot water or a small flame. Many automatic sprinklers, electric fuses, and safety devices in fire detection and suppression systems rely on such an alloy, tuned to melt at 47 °C.
Its other use leans on a quirk of chemistry: unlike its old look-alike lead, bismuth is essentially non-toxic. That makes it a replacement for lead in shot, bullets, and less-lethal riot gun ammunition. The European Union's restriction on lead has also widened its use in electronics. There it goes into low-melting-point solders that stand in for traditional tin-lead solders.

Bismuth compounds reach into the medicine cabinet and the makeup bag. Bismuth subsalicylate treats diarrhoea and is the active ingredient in "pink bismuth" preparations such as Pepto-Bismol. Bismuth oxychloride lends a pearly sheen to cosmetics, used as a pigment in eye shadows, hair sprays, and nail polishes.

Where it forms, where it's found

Geological setting

Low to high-temperature hydrothermal veins

2,030recorded occurrences
Source · OpenStreetMap

Varieties

Physical

Hardness
123456789102 – 2.5/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Transparency
Opaque
Colour
Lead gray to tin white

Yellowish or iridescent tarnish.

Streak
Lead-gray
Tenacity
flexible
Cleavage
Perfect

Perfect on (010) imperfect on (100) (110)

Somewhat sectile

Density
6.78 g/cm³

Optical

Anisotropism
Strong, especially in oil
Tropism
Anisotropic
Reflectance R%
(35.7, 46.2) 400, (36.4, 47.2) 420, (37.2, 47.9) 440, (37.7, 48.3) 460, (37.7, 48.8) 480, (37.6, 49.4) 500, (37.3, 49.6) 520, (37.1, 49.1) 540, (36.9, 48.7) 560, (36.8, 48.3) 580, (36.6, 47.8) 600, (36.4, 47.3) 620, (36.3, 46.8) 640, (36.1, 46.3) 660, (36.0, 45.8) 680, (35.9, 45.4) 700
Reflected-light panel
36.7 %anisotropic · dual curve
Specimen sRGB 216, 152, 84
White reference100 % reflector under same lamp
R₁ R₂
Mode
Anisotropism
Strong, especially in oil

Crystallography

Crystal system
Orthorhombic
Space group
#71
Cell parameters
a = 11.12 Å · b = 11.25 Å · c = 3.97 Å
Ratio a:b:c
1 : 1.012 : 0.357
Z
4
Morphology

Stout prismatic to acicular.

Comment

Space group Pbnm.

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
83BiBismuthBismuth2208.980417.960
81.29%
16SSulfurSulfur332.06096.180
18.71%
Total514.140100.00%

Mass share = atoms × atomic mass ÷ molar mass × 100

From IMA formula

Impurities
  • Pb
  • Cu
  • Fe
  • As
  • Sb
  • Se
  • Te

Synonyms

  • Bismuth Glance
  • Bismuthine
  • Bismutholamprite
  • Bizmutyn
  • Wismutglanz

In other languages

French
12233-37-3 · Bismuthine · Bismuthinite · Bismutholamprite · Bismutinite · Cheleutite · Csiklovaite · Horobetsuite
German
Bismutglanz · Bismuthin · Bismuthinit · Bismutin · Wismutglanz
Spanish
Bismutina · Bismutinita
Italian
bismutinite
Japanese
輝蒼鉛鉱
Chinese
辉铋矿
Russian
Bi2S3 · Бисмутин · Висмутин · Висмутинит · Висмутовый блеск

Classification

Strunz
10th ed.

2.DB.05

  • 2Sulfides and SulfosaltsClass
  • 2.DMetal Sulfides, M: S = 3 :4 and 2:3Division
  • 2.DBM:S = 2:3Group
  • 2.DB.05BismuthiniteSpecies
Dana
8th ed.

02.11.02.03

  • 02SulfidesClass
  • 02.11AmBnXp, with (m+n):p = 2:3Type
  • 02.11.02Stibnite Group (Orthorhombic: Pbnm)Group
  • 02.11.02.03BismuthiniteSpecies
CIM

3.7.17

  • 3Sulphides, Selenides, Tellurides, Arsenides and Bismuthides (except the arsenides, antimonides and bismuthides of Cu, Ag and Au, which are included in Section 1)Class
  • 3.7Sulphides etc. of V, As, Sb and BiGroup
  • 3.7.17BismuthiniteSpecies

Group, growth & confusion

In the same group
3 members
Often grow together
18 minerals
Commonly confused with
1 mineral

Literature, links & citation

Citations
  1. 1827Phillips, William (1827) Ueber die Krystallform des natürlichen und künstlichen Schwefelwismuths. Annalen der Physik und Chemie, 87. 476-478 doi:10.1002/andp.18270871113DOI: 10.1002/andp.18270871113
  2. 1827Phillips, W. (1827) On the crystalline forms of the natural and artificial sulphuret of bismuth. The Philosophical Magazine: 2: 181-182.
  3. 1830Beudant, François-Sulpice (1830) Traité élémentaire de minéralogie. Deuxiéme Edition [Elementary Treatise on Mineralogy. Second Edition] (2nd ed.) Vol. 1 - Tome Premier [Volume One]. Chez Verdière.
  4. 1854Rose, G. (1854) Ueber die Krystallform des künstlichen Schwefelwismuths. Annalen der Physik und Chemie, 167. 401-403 doi:10.1002/andp.18541670305DOI: 10.1002/andp.18541670305
  5. 1881Groth, P. (1881) Zeitschrift für Kristallographie: 5: 252.
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Bismuthinite — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/bismuthinite-686},
  note      = {Accessed 2026-05-11}
}