Skip to content
EntityQ413498· pop 37· linked from 80 articles

Acanthite is a form of silver sulfide with the chemical formula Ag2S. It crystallizes in the monoclinic system and is the stable form of silver sulfide below . Argentite is the stable form above that temperature. As argentite cools below that temperature its cubic form is distorted to the monoclinic form of acanthite. Below 173 °C acanthite forms directly. Acanthite is the only stable form in normal air temperature.

Key facts

Mineral.name
Acanthite
Mineral.category
Sulfide mineral
Mineral.image
Acanthite - Imiter mine, Jbel Saghro, Tinghir, Drâa-Tafilalet, Morocco.jpg
Mineral.imagesize
280px
Mineral.caption
Crystallized acanthite (4.0 × 2.5 × 1.5 cm) from Imiter mine, Jbel Saghro mountain range, Morocco
Mineral.formula
Ag2S
Mineral.IMAsymbol
Aca
Mineral.strunz
2.BA.30a
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/n
Mineral.unit cell
a = 4.229 Å, b = 6.931 Å c = 7.862 Å; β = 99.61°; Z = 4
Mineral.color
Iron-black
Mineral.habit
Primary crystals rare, prismatic to long prismatic, elongated along [001], may be tubular; massive. Commonly paramorphic after the cubic high-temperature phase ("argentite"), of original cubic or octahedral habit
Mineral.twinning
Polysynthetic on {111}, may be very complex due to inversion; contact on {101}
Mineral.cleavage
Indistinct
Mineral.fracture
Uneven
Mineral.tenacity
Sectile

via Wikipedia infobox

~3 min read

Encyclopedic overview

4 sections
Contents
  • Occurrence
  • Gallery
  • See also
  • References

{{infobox mineral | name = Acanthite | category = Sulfide mineral | boxwidth = | boxbgcolor = | image = Acanthite - Imiter mine, Jbel Saghro, Tinghir, Drâa-Tafilalet, Morocco.jpg | imagesize = 280px | alt = | caption = Crystallized acanthite (4.0 × 2.5 × 1.5 cm) from Imiter mine, Jbel Saghro mountain range, Morocco | formula = Ag2S |IMAsymbol=Aca | molweight = | strunz = 2.BA.30a | dana = | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/n | unit cell = a = 4.229 Å, b = 6.931 Å c = 7.862 Å; β = 99.61°; Z = 4 | color = Iron-black | colour = | habit = Primary crystals rare, prismatic to long prismatic, elongated along [001], may be tubular; massive. Commonly paramorphic after the cubic high-temperature phase ("argentite"), of original cubic or octahedral habit | twinning = Polysynthetic on {111}, may be very complex due to inversion; contact on {101} | cleavage = Indistinct | fracture = Uneven | tenacity = Sectile | mohs = 2.0–2.5 | luster = Metallic | streak = Black | diaphaneity = Opaque | gravity = 7.20–7.22 | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence= | absorption = | melt = | fusibility = | diagnostic = | solubility = | other = | alteration = | references = }} Acanthite is a form of silver sulfide with the chemical formula Ag2S. It crystallizes in the monoclinic system and is the stable form of silver sulfide below . Argentite is the stable form above that temperature. As argentite cools below that temperature its cubic form is distorted to the monoclinic form of acanthite. Below 173 °C acanthite forms directly. Acanthite is the only stable form in normal air temperature.

==Occurrence== Acanthite is a common silver mineral in moderately low-temperature hydrothermal veins and in zones of supergene enrichment. It occurs in association with native silver, pyrargyrite, proustite, polybasite, stephanite, aguilarite, galena, chalcopyrite, sphalerite, calcite and quartz.

Excerpted from Wikipedia’s “acanthite” article, available under the CC BY-SA 4.0 licence.