Rock Identifier
Dragon blood jasper (Epidote- and piemontite-bearing quartz/chalcedony (trade name)) — mineral
mineral

Dragon blood jasper

Epidote- and piemontite-bearing quartz/chalcedony (trade name)

AI-generated identification · may be incorrect

Typically hardness 6.5–7 Mohs, opaque, green matrix with red epidote or piemontite patches, and a vitreous to waxy polished luster; cryptocrystalline quartz lacks visible cleavage. Specific gravity is commonly about 2.6–2.8.

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Physical properties

Typically hardness 6.5–7 Mohs, opaque, green matrix with red epidote or piemontite patches, and a vitreous to waxy polished luster; cryptocrystalline quartz lacks visible cleavage. Specific gravity is commonly about 2.6–2.8.

Formation & geological history

A decorative jasper formed when silica-rich fluids replaced or cemented volcanic rock, incorporating green epidote/chlorite and red iron- or manganese-bearing minerals; specimens are generally associated with ancient metamorphosed volcanic terrains. Commonly marketed from Western Australia, especially the Pilbara region.

Uses & applications

Used for cabochons, tumbled stones, carvings, ornaments, and lapidary collections; it has modest gemstone 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 the name can vary considerably in composition.

Field identification & locations

Identify it by its polished green groundmass and irregular red blotches, opaque appearance, and lack of banding typical of many agates; confirm with hardness and specific-gravity tests. Common rough material comes from Australia and similar jasper deposits worldwide.