
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Iron Oxide inclusions
Hardness: 6.5-7 on Mohs scale; Color: Dark red to reddish-brown; Luster: Vitreous to dull (smooth polished finish); Crystal structure: Microcrystalline/Cryptocrystalline trigonal; Cleavage: None, conchoidal fracture; Specific gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Dark red to reddish-brown
- Luster
- Vitreous to dull (smooth polished finish)
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Dark red to reddish-brown; Luster: Vitreous to dull (smooth polished finish); Crystal structure: Microcrystalline/Cryptocrystalline trigonal; Cleavage: None, conchoidal fracture; Specific gravity: 2.58-2.91.
Formation & geological history
Formed as silica-rich fluids permeate micro-porous rocks or volcanic ash, absorbing iron oxide minerals (hematite) which give it its characteristic deep red hue.
Uses & applications
Commonly used for tumbled stones, cabochons, lapidary art, beads, ornamental carvings, and gemstone collections.
Geological facts
Red Jasper has been used since antiquity in seals, amulets, and decorative arts. It is known for its opaque, rich color caused by iron impurities embedded within the quartz matrix.
Field identification & locations
Identify by its opaque reddish-brown appearance, smooth tumbled texture, and high hardness (cannot be scratched by a steel knife). Commonly found in alluvial gravels, basalt flows, and sedimentary deposits worldwide (e.g., South Africa, Brazil, India, USA).
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