
metamorphic
Polished dragon blood jasper
Epidote–pistachio jasper (trade name; commonly quartz/chalcedony with epidote and red piemontite or iron oxides)
AI-generated identification · may be incorrectTypically opaque, moss-green with brick-red patches, waxy to glassy luster, and no visible cleavage; hardness about 6.5–7 Mohs, with a microcrystalline quartz groundmass and variable specific gravity near 2.6–3.3.
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Physical properties
Typically opaque, moss-green with brick-red patches, waxy to glassy luster, and no visible cleavage; hardness about 6.5–7 Mohs, with a microcrystalline quartz groundmass and variable specific gravity near 2.6–3.3.
Formation & geological history
Forms when silica-rich material is altered and cemented with epidote and iron- or manganese-bearing minerals, commonly in volcanic or metamorphic settings; exact age depends on locality. This specimen is tumbled and polished.
Uses & applications
Used for cabochons, carvings, beads, palm stones, and decorative objects; it has modest gemstone and lapidary value rather than fine-jewelry rarity.
Geological facts
“Dragon blood jasper” is a commercial name, not a formally defined mineral species, and material sold under it can vary substantially in composition.
Field identification & locations
Identify it by the distinctive red-on-green pattern, opaque quartz-like surface, and ability to scratch glass; common trade sources include South Africa and Australia, though visual identification alone is not definitive.
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