Realgar

China
7.46 carats
© Rarestone.com
Realgar is named from Arabic "rahj al-gar" - powder of the mine, because it was found in a silver mine.
Realgar forms red to orange-yellow prismatic crystals or granular masses. The crystals disintegrate to a powder after long exposure to light. However, this process takes a very long time. Realgar specimens should be kept in the dark, in an eclosed container.
Realgar is a very rare gem. It is very soft and somewhat unstable.
| General Information |
|---|
| Chemical Formula | Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Physical Properties of Realgar |
|---|
| Mohs Hardness | 1.5 to 2Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Specific Gravity | 3.56Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Tenacity | Brittle,SectileAnthony et al, Handbook of mineralogy (2001) |
|---|
| Cleavage Quality | GoodAnthony et al, Handbook of mineralogy (2001) |
|---|
| Light Sensitivity | Disintegrate to a powder after long exposure to lightMichael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Optical Properties of Realgar |
|---|
| Refractive Index | 2.538 to 2.704Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Optical Character | Biaxial/-Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Birefringence | 0.166Michael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Pleochroism | Nearly colorless to pale golden yellowAnthony et al, Handbook of mineralogy (2001) |
|---|
| Dispersion | Very strongAnthony et al, Handbook of mineralogy (2001) |
|---|
| Colour |
|---|
| Colour (General) | Red to orange-yellowMichael O?Donoghue, Gems, Sixth Edition (2006) More from other references |
|---|
| Transparency | TransparentMichael O?Donoghue, Gems, Sixth Edition (2006) More from other references |
|---|
| Lustre | GreasyMichael O?Donoghue, Gems, Sixth Edition (2006) More from other references |
|---|
| Crystallography of Realgar |
|---|
| Crystal System | MonoclinicMichael O?Donoghue, Gems, Sixth Edition (2006) |
|---|
| Habit | PrismaticMichael O?Donoghue, Gems, Sixth Edition (2006) More from other references |
|---|
| Geological Environment |
|---|
| Where found: | Most commonly as a low-temperature hydrothermal vein mineral associated with As–Sb minerals; also as volcanic sublimations and in hot spring deposits; in carbonate and clay.
sedimentary rocksAnthony et al, Handbook of mineralogy (2001) |
| Further Information |
|---|
| Mineral information: | Realgar information at mindat.org |
|---|
| Significant Gem Localities |
|---|
| Peru | | |
| | | USA | | |
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 442 | |
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 442 | |
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 442 |
|
|