
sedimentary
Jasper
Silicon dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Reddish-brown, yellow, and tan due to iron inclusions; Luster: Dull to greasy; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown, yellow, and tan due to iron inclusions
- Luster
- Dull to greasy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Reddish-brown, yellow, and tan due to iron inclusions; Luster: Dull to greasy; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of fine-grained silica-rich sediments or volcanic ash that undergo lithification. Often found as nodules or fillings in cracks and cavities within volcanic or sedimentary rocks over millions of years.
Uses & applications
Commonly used for lapidary work, jewelry making (cabochons), ornamental decoration, and as a collector's specimen.
Geological facts
Jasper is an opaque variety of chalcedony. Its colors are primarily derived from the oxidation of iron minerals within the stone. In ancient times, jasper was believed to provide physical strength and protection to the wearer.
Field identification & locations
Identify in the field by its opacity (it will not let light through even at thin edges, unlike quartz), its waxy feel when polished, and its characteristic smooth, curved fractures. Found in riverbeds and mountainous regions globally.
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