Cinnabar is the most common mercury mineral. It has a scarlet color. It is an important ore of mercury. In ancient times it was used for the production of red paint. Crystals are characterized by the formation of germination twins. But as a rule, cinnabar is found in the form of continuous masses. Large crystals are rare. Can be melted at only 200 degrees.
You can see cinnabar stone for sale and buy it in the Minerals of Russia online store.
General | |
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Category | Sulfide mineral |
Formula (repeating unit) |
Mercury(II) sulfide, HgS |
IMA symbol | Cin |
Strunz classification | 2.CD.15a |
Crystal system | Trigonal |
Crystal class | Trapezohedral (32) (same H–M symbol) |
Space group | P3121, P3221 |
Unit cell | a = 4.145(2) Å, c = 9.496(2) Å, Z = 3 |
Identification | |
Color | Cochineal-red, towards brownish red and lead-gray |
Crystal habit | Rhombohedral to tabular; granular to massive and as incrustations |
Twinning | Simple contact twins, twin plane {0001} |
Cleavage | Prismatic {1010}, perfect |
Fracture | Uneven to subconchoidal |
Tenacity | Slightly sectile |
Mohs scale hardness | 2.0–2.5 |
Luster | Adamantine to dull |
Streak | Scarlet |
Diaphaneity | Transparent in thin pieces |
Specific gravity | 8.176 |
Optical properties | Uniaxial (+) |
Refractive index | nω = 2.905 nε = 3.256 |
Birefringence | δ = 0.351 |
Solubility | 1.04×10−25 g/100 ml water (Ksp at 25 °C = 2×10−32) |