Erythrite: Difference between revisions
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{{short description|A hydrated cobalt arsenate mineral}} | |||
{{mineral}} | |||
== | ==Etymology== | ||
The name "erythrite" is derived from the Greek word "erythros," meaning red, in reference to its distinctive color. | |||
== | ==Chemical composition== | ||
Erythrite is | Erythrite is a secondary [[hydrated cobalt arsenate]] mineral with the chemical formula Co_(AsO_)_·8H_O. It forms as a result of the oxidation of primary cobalt minerals. | ||
== | ==Physical properties== | ||
Erythrite is | Erythrite typically forms in the [[monoclinic crystal system]] and is known for its striking pink to red color, which is due to the presence of cobalt. It has a [[Mohs hardness]] of 1.5 to 2.5, making it relatively soft. The mineral exhibits a pearly to vitreous luster and has a specific gravity of approximately 3.1. | ||
== | ==Occurrence== | ||
Erythrite | Erythrite is commonly found in the oxidized zones of cobalt and nickel deposits. It is often associated with other secondary minerals such as [[annabergite]], [[scorodite]], and [[cobaltite]]. Notable localities include the [[Bou Azzer District]] in Morocco, the [[Cobalt District]] in Ontario, Canada, and the [[Blackbird Mine]] in Idaho, USA. | ||
== | ==Uses== | ||
While erythrite itself is not a major ore of cobalt, it serves as an important indicator mineral for the presence of cobalt deposits. Its vibrant color also makes it a popular specimen among mineral collectors. | |||
== | ==Gallery== | ||
[[File:Erythrite-176702.jpg|thumb|right|Erythrite specimen showing its characteristic pink color.]] | |||
==Related pages== | |||
* [[Cobaltite]] | |||
* [[Annabergite]] | |||
* [[Scorodite]] | |||
* [[Mineral collecting]] | |||
[[Category:Arsenate minerals]] | [[Category:Arsenate minerals]] | ||
[[Category:Cobalt minerals]] | |||
[[Category:Monoclinic minerals]] | |||
Latest revision as of 10:51, 15 February 2025
A hydrated cobalt arsenate mineral
Etymology[edit]
The name "erythrite" is derived from the Greek word "erythros," meaning red, in reference to its distinctive color.
Chemical composition[edit]
Erythrite is a secondary hydrated cobalt arsenate mineral with the chemical formula Co_(AsO_)_·8H_O. It forms as a result of the oxidation of primary cobalt minerals.
Physical properties[edit]
Erythrite typically forms in the monoclinic crystal system and is known for its striking pink to red color, which is due to the presence of cobalt. It has a Mohs hardness of 1.5 to 2.5, making it relatively soft. The mineral exhibits a pearly to vitreous luster and has a specific gravity of approximately 3.1.
Occurrence[edit]
Erythrite is commonly found in the oxidized zones of cobalt and nickel deposits. It is often associated with other secondary minerals such as annabergite, scorodite, and cobaltite. Notable localities include the Bou Azzer District in Morocco, the Cobalt District in Ontario, Canada, and the Blackbird Mine in Idaho, USA.
Uses[edit]
While erythrite itself is not a major ore of cobalt, it serves as an important indicator mineral for the presence of cobalt deposits. Its vibrant color also makes it a popular specimen among mineral collectors.
Gallery[edit]
