
sedimentary
Red Jasper with Quartz Veins
Microcrystalline Quartz (SiO2) with Ferric Oxide (Fe2O3) inclusions
Hardness: 6.5-7 on Mohs scale; Color: Maroon/Brick red with white to tan veins; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Maroon/Brick red with white to tan veins
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Maroon/Brick red with white to tan veins; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed via the deposition of silica-rich sediments or volcanic ash where iron impurities provide the red pigmentation. The white quartz veins formed later through hydrothermal processes, where silica-saturated water filled fractures in the existing rock and crystallized.
Uses & applications
Used primarily for lapidary work including cabochons, beads, and stone carvings. Also popular in landscaping and as decorative 'pocket stones' or collector specimens.
Geological facts
Red Jasper has been used since ancient times for amulets and seals. It is often referred to as a 'stone of endurance.' The white veins seen here create a variety often called 'Zebra Jasper' or simply 'Veined Jasper'.
Field identification & locations
Identify in the field by its deep red color, hardness (it will scratch glass but cannot be scratched by a steel knife), and smooth, water-worn texture if found near riverbeds. Common in areas with ancient volcanic or sedimentary activity.
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