
sedimentary
Dragon Blood Jasper
Quartz (SiO2) with Epidote and Piedmontite inclusions
AI-generated identification · may be incorrectHardness: 6.5-7.0 on Mohs scale; Color: Forest green with deep red patches; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.6-2.9
- Hardness
- 6
- Color
- Forest green with deep red patches
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7.0 on Mohs scale; Color: Forest green with deep red patches; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.6-2.9
Formation & geological history
Formed through the silicification of volcanic or sedimentary rocks, where silica-rich fluids permeate the host rock during low-grade metamorphism or hydrothermal activity. Often found in South Africa and Australia.
Uses & applications
Used primarily in jewelry (cabochons and beads), ornamental carvings, and as a popular meditation or lapidary stone for collectors.
Geological facts
Despite the name, it is not a true Jasper in the mineralogical sense but a member of the chalcedony family featuring green Epidote and red Piedmontite. Folklore suggests the red spots represent the blood of dragons and the green represent their scales.
Field identification & locations
Identified by its distinctive deep green base with maroon or red blotches. It is opaque and takes a high polish. Primarily sought after in South Africa (Limpopo) and Western Australia. Collectors look for high contrast between the red and green colors.
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