
sedimentary
Jasper
Jasper (Silicon Dioxide, SiO2)
Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown to maroon due to iron oxide impurities, Luster: Dull to waxy, Crystal Structure: Microcrystalline (Cryptocrystalline) hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.91
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown to maroon due to iron oxide impurities, Luster: Dull to waxy, Crystal Structure: Microcrystalline (Cryptocrystalline) hexagonal, 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 (mostly sedimentary origins, occasionally metamorphic). Iron oxides provide the deep red pigment. Often found in Precambrian formations.
Uses & applications
Used widely in lapidary work, jewelry (cabochons, beads), decorative ornaments, and as a durable material for historical tools like scrapers and arrowheads.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek 'iaspis', meaning 'spotted stone.' It has been used historically as a gemstone and for ritualistic purposes by numerous ancient cultures including the Babylonians and Egyptians.
Field identification & locations
Identify in the field by its opaque nature (unlike translucent carnelian), conchoidal fracture, and inability to be scratched by a steel knife. Commonly found in riverbeds, glacial deposits, or near volcanic regions. Proving ground: Western USA (Oregon, Idaho), India, and Brazil.
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