
sedimentary
Jasper
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Red, brown, yellow, or green (often mottled); Luster: Vitreous to dull; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None; Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Red, brown, yellow, or green (often mottled)
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Red, brown, yellow, or green (often mottled); Luster: Vitreous to dull; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None; Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica-rich fluids within cracks or volcanic ash, typically in sedimentary environments where iron oxides and other minerals provide pigmentation. It can range from Precambrian to recent geological ages.
Uses & applications
Primarily used for lapidary work, jewelry (cabochons, beads), decorative ornaments, and as a popular specimen for crystal collecting and metaphysical purposes.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'Jasper' is derived from the Greek word 'iaspis', meaning 'spotted stone.' Many varieties are named after their appearance, such as 'Ocean Jasper' or 'Leopard Skin Jasper.'
Field identification & locations
Identify in the field by its opacity (it does not transmit light even on thin edges), its smooth conchoidal fracture, and extreme hardness. Common locations include India, Brazil, Madagascar, and the United States (specifically Oregon and Idaho).
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