
sedimentary
Red Jasper (River Pebble)
Silicon Dioxide (SiO2) with Hematite impurities
Hardness: 6.5-7 (Mohs scale); Color: Opaque brick red to brownish-red; Luster: Dull to sub-vitreous; Crystal Structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Opaque brick red to brownish-red
- Luster
- Dull to sub-vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Opaque brick red to brownish-red; Luster: Dull to sub-vitreous; Crystal Structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or volcanic ash, occurring within sedimentary or volcanic environments. This specific specimen has been smoothed and rounded by long-term water erosion in a river or beach setting.
Uses & applications
Commonly used for lapidary work, jewelry (cabochons, beads), decorative tumbled stones, and as a healing stone in metaphysical practices.
Geological facts
Red jasper has been used for thousands of years; Ancient Egyptians associated it with the blood of Isis and used it in amulets. Its red color is derived from high concentrations of iron oxide (Hematite).
Field identification & locations
Identify by its opaque red color, smoothness from water wear, and inability to be scratched by a steel knife. It is commonly found in gravel beds, riverbanks, and coastlines worldwide.
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