
sedimentary
Jasper
Silicon dioxide (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown due to iron inclusions; Luster: Dull to vitreous; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91.
- Hardness
- 6
- Color
- Reddish-brown due to iron inclusions
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown due to iron inclusions; Luster: Dull to vitreous; 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, the silica crystallizes and incorporates mineral impurities that provide the characteristic color. Most specimens range from millions to hundreds of millions of years old.
Uses & applications
Commonly used for lapidary work, cabochons, beads for jewelry, and ornamental stones. Historically used for making tools like scrapers and arrowheads due to its hardness and sharp fracture edges.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek word 'iaspis', meaning 'spotted stone'. It was one of the stones in the breastplate of the Jewish high priest in the Old Testament.
Field identification & locations
Identify in the field by its opaque nature (unlike agate, light will not pass through it even on thin edges) and its smooth, waxy surface when water-worn. Common in riverbeds and coastal regions where volcanic or sedimentary layers have eroded.
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