
sedimentary
Jasper
Silicon dioxide (SiO2)
Hardness: 6.5-7 (Mohs); Color: Brown, tan, reddish-brown; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brown, tan, reddish-brown
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Brown, tan, reddish-brown; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine-grained sediments. Over time, these fluids solidify into a dense, opaque variety of chalcedony. The brown colors are typically due to iron oxides (like goethite or limonite).
Uses & applications
Used primarily as a gemstone for jewelry (cabochons), lapidary art, ornaments, and historical tools like scrapers and arrowheads due to its hardness.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'jasper' comes from the Greek word 'iaspis', meaning 'spotted stone.' Some varieties are so distinct they are named after their location, like Owyhee Jasper or Mookaite.
Field identification & locations
Identify in the field by its opaque nature (unlike translucent agate), conchoidal fracture (curved breaks), and the fact that it cannot be scratched by a steel knife. Frequently found in riverbeds, deserts, and volcanic regions.
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