Cinnabar

cinnabar

stibnite

smithsonite

realgar

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Formula: HgS
Sulphide
Crystal System: Trigonal
Specific gravity: 8.176 measured, 8.20 calculated
Hardness: 2 2½
Streak: Red
Colour: Red
Solubility: Insoluble in hydrochloric acid, sulphuric and nitric acid
Environments:

Metamorphic environments
Hydrothermal environments
Fumeroles and Hot Spring deposits

Cinnabar occurs in the oxidation zone of epithermal (low temperature) hydrothermal veins, at fumeroles, and also in hot springs. It may be associated with baryte, native mercury, pyrite, marcasite, opal, quartz, realgar, stibnite, and sulphides of copper. Cinnabar is the most important ore of mercury but is found in quantity at comparatively few locations.

At the Rutland Cavern, Heights of Abraham, Matlock Bath, Derbyshire, England, UK, cinnabar has been found associated with smithsonite, and as minute specks dusting the surface of both smithsonite and fluorite (RES p51).

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