Native Arsenic

As
IMA status
  • Approved
  • Grandfathered
IMA symbol
As
Also known as

History

The name carries an old insult. It comes through Greek as arsenikon, a word that meant masculine or virile, chosen to flag the mineral's potent nature. The Greek term itself traces back through Arabic al-zarnīḵ, "the orpiment", and ultimately to a Persian root for gold — orpiment being a golden-yellow arsenic mineral. The earliest written record of the English word sits in a 1310 account of orpiment sold by the pound, its author unknown.

Long before chemists could isolate the element, people knew its golden and red sulfides — orpiment and realgar — as pigments and as poisons. Around 300 CE the alchemist Zosimos roasted realgar to drive off a "cloud of arsenic", arsenic trioxide, then reduced that to a grey metal. The Persian alchemist Jabir ibn Hayyan described separating arsenic before 815 CE, and Albertus Magnus isolated the element in 1250 by heating arsenic trisulfide with soap.

A poison and a pigment

Few minerals carry a darker human record. Arsenic earned the names poison of kings and king of poisons, and the inheritance powder — a tasteless white powder, arsenic trioxide, used to hurry along wealthy relatives in Renaissance Europe.

The same element gave painters two brilliant greens. Scheele's Green arrived in 1775 and Paris Green in 1814, and both spread through Victorian wallpapers, fabrics, and paints. Victorian women even ate white arsenic mixed with vinegar and chalk to pale their complexions.

Medicine reached for it too. Through the 17th, 18th, and 19th centuries arsenic compounds treated diseases such as cancer and psoriasis — among them Fowler's solution and the drug arsphenamine developed by Paul Ehrlich.

The native element itself stayed scarce. Crystals of native arsenic do form in nature, but only rarely. One documented source is Sainte-Marie-aux-Mines in eastern France.

Industrial & practical applications

Almost none of the arsenic that industry consumes comes from the native mineral. The metal is rare in its native form. Producers recover it instead as a by-product of smelting other ores — chiefly the iron-arsenic-sulfur mineral arsenopyrite, and the dust left by copper, gold, and lead smelting. Arsenic is in fact the main impurity in the copper concentrates fed to smelters, and most of it is recovered from copper-refinement dust. Everything below draws on that smelter-derived supply, not on crystals of native arsenic.

The largest single use is alloying with lead. A trace of arsenic stiffens the lead grids inside car batteries, helping them hold their shape. As much as 2% of all arsenic produced goes into the lead alloys used for shot and bullets. Arsenic is also added to brass — a copper-zinc alloy — where it sharply slows dezincification, the corrosion that leaches zinc out and weakens the metal.

In electronics, arsenic combines with gallium to make gallium arsenide, a semiconductor used in integrated circuits. Circuits built from it run much faster than silicon ones, though they cost far more. Because the material has a direct bandgap — it can turn electrical energy straight into light — it also drives laser diodes and light-emitting diodes.

A warning runs through all of it. Every form of arsenic is a serious risk to human health, and the element is classed as a group 1 carcinogen, the category for substances known to cause cancer in humans. Native arsenic specimens warrant the same caution: handle them as you would any toxic material, and wash your hands afterward.

Where it forms, where it's found

Geological setting

Hydrothermal veins.

383recorded occurrences
Source · OpenStreetMap

Safety & handling

Physical

Hardness
123456789103.5/ 10 MOHS
  1. 1Talc
  2. 2Gypsum
  3. 3Calcite
  4. 4Fluorite
  5. 5Apatite
  6. 6Orthoclase
  7. 7Quartz
  8. 8Topaz
  9. 9Corundum
  10. 10Diamond
Lustre
Metallic
Transparency
Opaque
Colour
Tin-white · tarnishing to dark grey or black.
Streak
Grey
Tenacity
brittle
Cleavage
Perfect

Perfect basal on (0001), fair on (0114)

Fracture
Irregular/Uneven
Density
5.63 g/cm³

Optical

Pleochroism
Weak
Anisotropism
Distinct - yellowish brown and light grey to yellowish grey
Tropism
Anisotropic
Reflectance R%
(56.0, 57.5) 400, (55.1, 56.8) 420, (54.2, 56.2) 440, (53.3, 55.8) 460, (52.7, 55.7) 480, (52.4, 55.7) 500, (52.0, 55.7) 520, (51.7, 55.7) 540, (51.5, 55.6) 560, (51.2, 55.4) 580, (51.0, 55.2) 600, (50.8, 55.0) 620, (50.6, 54.9) 640, (50.5, 54.8) 660, (50.4, 54.7) 680, (50.4, 54.6) 700
Luminescence
None
UV response
Not fluorescent in UV
Reflected-light panel
52.1 %anisotropic · dual curve
Specimen sRGB 250, 176, 101
White reference100 % reflector under same lamp
R₁ R₂
Mode
Anisotropism
Distinct - yellowish brown and light grey to yellowish grey

Crystallography

Crystal system
Trigonal
Space group
R-3m
Cell parameters
a = 3.768 Å · c = 10.574 Å
Z
6
Morphology

Granular, massive, concentric layered. Reticulated, reniform, stalagtitic, columnar, acicular. small rhombohedra.

Twinning

Rare on (1014), Pressure twinning on (0112)

Crystal structure

Chemical composition

Constituent elements
Mass composition breakdown
ElementAtoms At. mass g/mol Mass g/molMass share
33AsArsenicArsenic174.92274.922
100.00%
Total74.922100.00%

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

From IMA formula

Impurities
  • Bi
  • Sb
  • Fe
  • Ni
  • Ag
  • S
  • Se

Synonyms

  • Arsanaic
  • Arseen
  • Arseeni
  • Arsen
  • Arsenas
  • Arsenico
  • Arsénico
  • Arsenicu
  • Arsènicu
  • Arsenicum
  • Arsenig
  • Arsenik
  • Arseniko
  • Arsênio
  • Arseno
  • Arsēns
  • Arsiniku
  • Arsnick
  • Artseniko
  • Arzen
  • Arzén
  • Asen
  • Asenia
  • Asenik
  • Löffelkobalt
  • Margimush
  • Scherbenkobalt
  • Αρσενικό
  • ஆர்சனிக்
  • ആര്‍സെനിക്

In other languages

French
Arsenic natif
German
Arsen, gediegen
Spanish
Arsénico nativo
Italian
arsenico nativo
Japanese
自然ヒ素 · 自然砒 · 自然砒素
Russian
мышьяк самородный · Самородный мышьяк

Classification

Strunz
10th ed.

1.CA.05

  • 1ElementsClass
  • 1.CMetalloids and NonmetalsDivision
  • 1.CAArsenic group elementsGroup
  • 1.CA.05Native ArsenicSpecies
Dana
8th ed.

01.03.01.01

  • 01Native Elements and AlloysClass
  • 01.03Semi-metals and non-metalsType
  • 01.03.01Arsenic groupGroup
  • 01.03.01.01Native ArsenicSpecies
CIM

1.33

  • 1Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and Au)Class
  • 1.33— unnamed intermediate level —Group
  • 1.33Native ArsenicSpecies

Group, growth & confusion

In the same group
3 members
Often grow together
13 minerals
Commonly confused with
2 minerals

Literature, links & citation

Citations
  1. https://en.wikipedia.org/wiki/Allotropes_of_arsenic
  2. 1789Hoffmann, C.A.S. (1789) Mineralsystem des Herrn Inspektor Werners mit dessen Erlaubnis herausgegeben von C.A.S. Hoffmann. Bergmännisches Journal, 2 (1) 369-398
  3. 1931Broderick, S. J., Ehret, W. F. (1931) An X-Ray Study of the Alloys of Silver with Bismuth, Antimony and Arsenic. II. The Journal of Physical Chemistry, 35 (11). 3322-3329 doi:10.1021/j150329a017DOI: 10.1021/j150329a017
  4. 1944Palache, Charles, Berman, Harry, Frondel, Clifford (1944) The System of Mineralogy (7th ed.) Vol. 1 - Elements, Sulfides, Sulfosalts, Oxides. John Wiley and Sons, New York.
  5. 1969Ramdohr, Paul (1969) The Ore Minerals and their Intergrowths. Pergamon Press, Oxford. 1174pp. doi:10.1016/c2013-0-10027-xDOI: 10.1016/c2013-0-10027-x
Cite this entry
@misc{mineral2026,
  author    = {Mineral Index editorial board},
  title     = {Native Arsenic — Mineral Index},
  year      = {2026},
  url       = {https://mineralindex.org/minerals/native-arsenic-357},
  note      = {Accessed 2026-05-11}
}