
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Deep brick red to brownish-red; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Deep brick red to brownish-red
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Deep brick red to brownish-red; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91.
Formation & geological history
Formed primarily in sedimentary environments where silica-rich fluids permeate through volcanic ash or sediment. The red color is derived from high concentrations of iron oxide (hematite) during the mineralization process.
Uses & applications
Used extensively in jewelry (cabochons, beads), decorative lapidary work, ornaments, and as a collector's gemstone. Historically used for seals and amulets.
Geological facts
Red Jasper was known as the 'stone of endurance' in ancient cultures and was frequently used by Viking and Germanic warriors to inlay the hilts of their swords for protection and courage.
Field identification & locations
Identify by its characteristic dull red color, heavy weight compared to common rocks, and smooth, shell-like (conchoidal) fracture patterns when broken. Commonly found in riverbeds and desert regions globally, particularly in the Western US, India, and Brazil.
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