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At the same time, Jameson believed that cobalt ochres have a lot in common and can be classified as a special class of minerals. ″The Black, Brown and Yellow Cobalt Ochres, and other similar minerals, ought to be arranged together, and form a particular order by themselves. In the mean time, we place them beside the Red Cobalt, on account of their being often associated with that mineral″.<ref name="robert">'']''. A System of Mineralogy, in which Minerals are Arranged According to the Natural History Method. Vol.2. — Edinburgh, A. Constable & Co., 1820.</ref>{{rp|197}} However, from a chemical point of view, Jameson and his contemporaries reduced the entire diversity of cobalt ochres to two groups of chemical compounds of cobalt: ] (]) and arsenates (]) in different morphological forms of ] and with a different set of impurities. At the same time, Jameson believed that cobalt ochres have a lot in common and can be classified as a special class of minerals. ″The Black, Brown and Yellow Cobalt Ochres, and other similar minerals, ought to be arranged together, and form a particular order by themselves. In the mean time, we place them beside the Red Cobalt, on account of their being often associated with that mineral″.<ref name="robert">'']''. A System of Mineralogy, in which Minerals are Arranged According to the Natural History Method. Vol.2. — Edinburgh, A. Constable & Co., 1820.</ref>{{rp|197}} However, from a chemical point of view, Jameson and his contemporaries reduced the entire diversity of cobalt ochres to two groups of chemical compounds of cobalt: ] (]) and arsenates (]) in different morphological forms of ] and with a different set of impurities.

== Essential minerals ==
* ]<ref name="kriv"/>{{rp|172}} — a secondary mineral of the ] with the formula (Со,Ni)O•MnO<sub>2</sub>•nH<sub>2</sub>O, consisting of hydrous oxides of ], ] and ]. Forms sooty, earthy masses (asbolan from the {{langx|grc|ασβολος}} — ]) of dirty colors from yellowish-brown to bluish-black.
* ]<ref name="kriv"/>{{rp|172}} — a secondary mineral of the ] class with the ideal formula Co<sub>3</sub>(AsO<sub>4</sub>)<sub>2</sub>•8(H<sub>2</sub>O), consisting of {{ill|cobalt(II) arsenate|ru|Арсенат кобальта(II)}} and usually also containing impurities of ], ], ], ] and ]. Due to its bright color, it is used as an indicator of nearby ] ores, and sometimes also ].

== Cobalt ochres gallery ==
<br>
<gallery>
Asbolan formerly Asbolite on serpentine Hydrous manganese cobalt oxide Porterville Tulate County California 2234.jpg|{{center|]}}
Erythrite-197790.jpg|{{center|]}}
</gallery>

== See also ==
* ]
* ]
* ]
* ]
* ]


== References == == References ==

Revision as of 15:45, 1 January 2025

Secondary cobalt minerals
Cobalt ochre
Erythrite (Sonora, Mexico)
General
CategoryMineral
For other uses, see Ochre (disambiguation).

Cobalt ochre, cobalt-ochre (Cobalt ocher in American English) or ochre of cobalt (German: Erdkobalt) — a common name that was widely used in mining and craft environments until the end of the 19th century for at least two cobalt-containing secondary ore minerals: asbolane and erythrite. They were often used with the addition of a clarifying color adjective or a clarifying mineral form adjective to avoid confusion.

For example, Robert Jameson divided cobalt ochres into four classes: black cobalt-ochres, brown cobalt-ochres, yellow cobalt-ochres and red cobalt-ochres. In turn, each of the color forms of ochre had two or three varieties. Black cobalt ochre had two main forms, which were widely distributed in the mines of Europe: earthy black cobalt-ochre and indurated black cobalt-ochre. Brown or yellow-brown cobalt-ochres varied in composition, sometimes being a mixture of black and yellow cobalt ochres. Yellow cobalt-ochres often appeared in association with various forms of red cobalt-ochres, as well as nickel ochres. Finally, red cobalt ochre was known in three mineral forms: earthy red cobalt-ochre, radiated red cobalt-ochre, and slaggy red cobalt-ochre.

At the same time, Jameson believed that cobalt ochres have a lot in common and can be classified as a special class of minerals. ″The Black, Brown and Yellow Cobalt Ochres, and other similar minerals, ought to be arranged together, and form a particular order by themselves. In the mean time, we place them beside the Red Cobalt, on account of their being often associated with that mineral″. However, from a chemical point of view, Jameson and his contemporaries reduced the entire diversity of cobalt ochres to two groups of chemical compounds of cobalt: oxides (asbolane) and arsenates (erythrite) in different morphological forms of crystallization and with a different set of impurities.

Essential minerals

Cobalt ochres gallery


See also

References

  1. ^ Krivovichev V. G. Mineralogical glossary. Scientific editor A. G. Bulakh. — St.Petersburg: St.Petersburg Univ. Publ. House. 2009. — 556 p. — ISBN 978-5-288-04863-0
  2. ^ Robert Jameson. A System of Mineralogy. Vol.3: Class IV. Metallic Minerals. — Edinburgh, A. Constable & Co., 1816.
  3. The Edinburgh Encyclopaedia, 1st American ed., Volume 13. J. and E. Parker edition, 1832.
  4. Robert Jameson. A System of Mineralogy, in which Minerals are Arranged According to the Natural History Method. Vol.2. — Edinburgh, A. Constable & Co., 1820.
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