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Acanthite

 

Acanthite

 

Discovered in 1783; IMA status: Valid (pre-IMA; Grandfathered)

 

Chemistry

 

 

Chemical Formula:

Ag2S

 

Silver Sulfide

Molecular Weight:

247.80 gm

Composition:

Silver

87.06 %

Ag

 

 

 

Sulfur

12.94 %

S

 

 

 

 

100.00 %

 

 

 

 

 

Classification

   

   

Mineral Classification:

Sulfides and Sulfosalts

Strunz 8th Ed. ID:

2/B.05-10

Nickel-Strunz 10th Ed. ID:

2.BA.35

 

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
B : Metal Sulfides, M: S > 1: 1 (mainly 2: 1)
A : With Cu, Ag, Au

Related to:

Acanthite Group. Isostructural with Aguilarite. Acanthite is the low-temperature version of Argentite.

Members of Group:

Acanthite Group: Acanthite, Aguilarite, Cervelleite

Varieties:

Zincian Acanthite

Synonyms:

Acantite, Akanthite, α-Argentite, Argentite, Argentite-beta, Argentite-β, Argyrite, Argyrose, Beta-Argentite, β-Argentite, Daleminzite, Henkelite, ICSD 30445, Para-Silberglanz, PDF 14-72, Silver Glance, Vitreous Silver

 

 

Crystal Data

   

   

Crystallography:

Monoclinic - Prismatic

Crystal Habit:

Primary crystals are rare, prismatic to long prismatic, elongated along [001], to 2.5 cm, may be tubular; massive. Commonly paramorphic after the cubic high-temperature phase (“argentite”), of original cubic or octahedral habit, to 8 cm. 

Twinning:

Polysynthetic on {111}, may be very complex due to inversion; contact on {101}

 

 

Physical Properties

   

 

Cleavage:

Indistinct, none observed

Fracture:

Irregular/uneven, sub-conchoidal

Tenacity:

Sectile

Moh's Hardness:

2.0 - 2.5; Vickers: VHN100=21 - 25 kg/mm2

Density:

7.2 - 7.4 (g/cm3)

Luminescence:

None

Radioactivity:

Not Radioactive

 

 

Optical Properties

   

   

Color:

Lead grey, iron black

Transparency:

Opaque

Luster:

Metallic

Refractive Index:

R: (400) 32.8, (420) 32.9, (440) 33.0, (460) 33.1, (480) 33.0, (500) 32.7, (520) 32.0, (540) 31.2, (560) 30.5, (580) 29.9, (600) 29.2, (620) 28.7, (640) 28.2, (660) 27.6, (680) 27.0, (700) 26.4

Birefringence:

n/a (opaque)

Dispersion:

n/a

Pleochroism:

n/a

Anisotropism:

Weak

 

 

Occurances

   

   

Geological Setting:

A common silver species in moderately low-temperature hydrothermal sulfide veins, and in zones of secondary enrichment.

Common Associations:

Silver, Pyrargyrite, Proustite, Polybasite, Stephanite, Aguilarite, Galena, Chalcopyrite, Sphalerite, Calcite, Quartz

Common Impurities:

Se

Type Locality:

Jáchymov (St Joachimsthal), Jáchymov District (St Joachimsthal), Krušné Hory Mts (Erzgebirge), Karlovy Vary Region, Bohemia (Böhmen; Boehmen), Czech Republic

Year Discovered:

1855

View mineral photos:

Acanthite Mineral Photos and Locations

 

 

More Information

   

   

 

Mindat.org
Webmineral.com

 

 

Acanthite is a silver sulfide mineral and is one of the most important ores of Silver. Acanthite was named in 1855 by Gustav Adolf Kenngott from the Greek word akantha meaning thorn, in allusion to its crystal shape. The name Acanthite is often confused with, or used interchangably with, Argentite. Acanthite and Agrentite have the same chemistry, Ag2S, but different structures. Acanthite is the low-temperature form of Argentite. Acanthite has a monoclinic structure and is stable below 173 degrees Celsius while Argentite has an isometric structure and is only stable at temperatures above 173 degrees Celsius. All natural silver sulphide specimens (and gems) at room temperature are Acanthite. The tarnish on sterling silver is chemically the same as Acanthite.

Acanthite was named in 1855 by German mineralogist Gustav Adolf Kenngott (1818-1897) from the Greek word άκανθα (ákantha) meaning thorn, in allusion to its crystal shape. It was discovered in the Jáchymov District, Krušné Hory Mts, Karlovy Vary Region, Bohemia, Czech Republic.

Acanthite distribution: widespread in silver deposits. Localities for fine primary and paramorphic crystals include: from Jáchymov (Joachimsthal), Czech Republic [TL]. In Germany, at Freiberg, Schneeberg, Annaberg, and Marienberg, Saxony; and from St. Andreasberg, Harz Mountains. In Mexico, large paramorphs from Arizpe, Sonora; in the Rayas and other mines at Guanajuato; and from many mines in Zacatecas, Chihuahua, etc. In the USA, at Butte, Silver Bow County, Montana; Tonopah, Nye County, and the Comstock Lode, Virginia City, Storey County, Nevada. From various mines at Cobalt, Ontario, Canada. At Chañarcillo, south of Copiapó, Atacama, Chile.

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