
sedimentary
Jasper
Silicon dioxide (SiO2) with iron oxide inclusions
Hardness: 6.5-7 (Mohs); Color: Mottled reddish-brown, yellow, and grey; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Mottled reddish-brown, yellow, and grey
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Mottled reddish-brown, yellow, and grey; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water-rich solutions into volcanic ash or sedimentary rocks. Over geological time, the silica crystallizes into microcrystalline quartz, with mineral impurities providing the coloration.
Uses & applications
Primarily used as a gemstone for jewelry (cabochons, beads), decorative ornaments, stone carvings, and as a popular specimen for rock collectors.
Geological facts
Jasper has been used as a gemstone since antiquity; it was known in ancient Egypt, Greece, and Rome. Its name is derived from the Greek 'iaspis', meaning 'spotted stone.'
Field identification & locations
Identify in the field by its opacity (unlike translucent agate), waxy feel when polished, and characteristic multicolored mottling. Commonly found in riverbeds, volcanic regions, and sedimentary deposits worldwide.
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