
sedimentary
Jasper with Cinnabar (Dragon Blood Jasper variant)
Silicon Dioxide with Mercury Sulfide (SiO2 + HgS)
AI-generated identification · may be incorrectHardness: 6.5-7 (Quartz matrix), Color: Tan to brown base with bright red inclusions, Luster: Dull to earthy (waxy when polished), Crystal Structure: Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Quartz matrix), Color: Tan to brown base with bright red inclusions, Luster: Dull to earthy (waxy when polished), Crystal Structure: Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
Formation & geological history
Formed through the infiltration of hydrothermal fluids containing mercury sulfide (cinnabar) into microcrystalline quartz (jasper) or volcanic tuff. This process typically occurs in low-temperature hydrothermal veins.
Uses & applications
Primarily used as a lapidary material for cabochons, beads, and carvings. Historically, cinnabar was a source of mercury, though it is now mostly a collector's item or ornamental stone.
Geological facts
Cinnabar-colored rocks are often called 'Dragon Blood' or 'Cinnabar Jasper.' Because cinnabar contains mercury, these stones should be handled with care, especially during cutting or sanding to avoid inhaling dust.
Field identification & locations
Identify in the field by looking for bright, 'blood-red' streaks or patches within a hard, silica-rich matrix. It is commonly found near volcanic activity and hot springs. Common locations include Nevada (USA), China, and Mexico.
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