
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite inclusions
Hardness: 6.5-7 (Mohs); Color: Deep brick red per hematite content; Luster: Vitreous to waxy; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6-2.9.
- Hardness
- 6
- Color
- Deep brick red per hematite content
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Deep brick red per hematite content; Luster: Vitreous to waxy; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.6-2.9.
Formation & geological history
Formed through the deposition of silica-rich fluids in volcanic vents or sedimentary strata. The red color is caused by the inclusion of fine-grained iron oxides (Hematite) during the crystallization process. It can be found in formations dating back millions of years.
Uses & applications
Used primarily for semi-precious jewelry (beads, cabochons), lapidary art, decorative carvings, and as a popular stone for tumbling and meditation practices.
Geological facts
Jasper was a favorite gem in the ancient world; its name can be traced back in Hebrew, Assyrian, Persian, Greek, and Latin. It is often referred to as the 'Stone of Endurance' and 'Supreme Nurturer' in metaphysical circles.
Field identification & locations
Identify by its opaque quality (unlike carnelian which is translucent), its smooth conchoidal fracture, and extreme hardness (cannot be scratched by a steel knife). Commonly found in riverbeds or coastal areas in Oregon, California, India, and Brazil.
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