In today's article, we are going to delve into Acanthite, a relevant topic that has captured the attention of many people in recent times. Throughout this text, we will analyze different aspects of Acanthite, from its origins to its impact on today's society. We will immerse ourselves in its history, explore its implications in different areas and reflect on its importance in the current context. Acanthite is an exciting topic that deserves to be addressed from different perspectives, which is why in this article we aim to offer a broad and enriching vision of this matter. Join us on this fascinating exploration!
Acanthite | |
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General | |
Category | Sulfide mineral |
Formula (repeating unit) | Ag2S |
IMA symbol | Aca |
Strunz classification | 2.BA.30a |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/n |
Unit cell | a = 4.229 Å, b = 6.931 Å c = 7.862 Å; β = 99.61°; Z = 4 |
Identification | |
Color | Iron-black |
Crystal habit | Primary crystals rare, prismatic to long prismatic, elongated along , 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 scale hardness | 2.0–2.5 |
Luster | Metallic |
Streak | Black |
Diaphaneity | Opaque |
Specific gravity | 7.20–7.22 |
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 173 °C (343 °F). 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.
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.
Acanthite was first described in 1855 for an occurrence in the Jáchymov (Joachimsthal) district, Ore Mountains, Bohemia (today Karlovy Vary Region, Czech Republic). The name is from the Greek "akantha" meaning thorn or arrow, in reference to its crystal shape.