
sedimentary
Bloodstone
Heliotrope (Quartz SiO2 with Iron Oxide inclusions)
AI-generated identification · may be incorrectHardness: 6.5-7.0 (Mohs scale); Color: Dark green with red spots (iron oxide); Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58–2.64
- Hardness
- 6
- Color
- Dark green with red spots (iron oxide)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7.0 (Mohs scale); Color: Dark green with red spots (iron oxide); Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific gravity: 2.58–2.64
Formation & geological history
Formed at low temperatures through the precipitation of silica from groundwater in cavities of other rocks. The red spots are caused by inclusions of hematite (iron oxide). Most specimens date back to the Cretaceous period.
Uses & applications
Used primarily in jewelry (beads, cabochons, seals), ornamental carvings, and as a popular collector's stone. Historically used for amulets and signet rings.
Geological facts
Also known as Heliotrope, which means 'sun turner' in Greek. In the Middle Ages, the red spots were believed to be the blood of Christ, leading to its common name and significant religious value in Christian art.
Field identification & locations
Identified by its dark forest-green base color and distinct 'splatters' of red iron oxide. While it is predominantly found in India, significant deposits also exist in Brazil, China, Australia, and the USA. Collectors look for a high contrast between the green and red.
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