
sedimentary
Jasper (Willow Creek/Desert style)
Silicon Dioxide (SiO2) with iron and clay impurities
Hardness: 6.5-7 (Mohs scale); Color: Olive green, tan, and beige with banding; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.9.
- Hardness
- 6
- Color
- Olive green, tan, and beige with banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Olive green, tan, and beige with banding; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.9.
Formation & geological history
Formed from the deposition of silica from hydrothermal solutions or volcanic ash in sedimentary environments. Its patterns are often the result of mineral-rich fluids flowing through cracks and solidifying over millions of years.
Uses & applications
Primarily used in jewelry as cabochons, pendants, and beads. Also popular for decorative stone carvings, tumbling, and as a collector's specimen due to its unique patterns.
Geological facts
Jasper is a variety of chalcedony. The name comes from the Greek 'iaspis', meaning spotted stone. It was once believed to provide protection against evil spirits and to help bring rain in drought-stricken areas.
Field identification & locations
Identify in the field by its opacity (it does not transmit light even on thin edges), its hardness (it will scratch glass), and its characteristic smooth, shell-like fracture pattern. Common locations include the USA (Idaho, Oregon), South Africa, and Brazil.
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