
sedimentary
Jasper (specifically Red Jasper/Chert)
Silicon Dioxide (SiO2) with iron oxide inclusions
Hardness: 6.5-7 (Mohs scale); Color: Reddish-brown, earthy tones; Luster: Dull to waxy; Crystal Structure: Trigonal/Microcrystalline (cryptocrystalline quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown, earthy tones
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Reddish-brown, earthy tones; Luster: Dull to waxy; Crystal Structure: Trigonal/Microcrystalline (cryptocrystalline quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water-rich environments, often near volcanic activity or in sedimentary basins. The red color is caused by iron (hematite) impurities during the mineralization process over millions of years.
Uses & applications
Used primarily as decorative stone, gemstones for jewelry (cabochons), and lapidary art. Historically used for making tools due to its sharp conchoidal fracture.
Geological facts
Jasper has been used by humans for thousands of years; it was a favorite gem in the ancient world, mentioned in various religious texts and found in Minoan carvings dating back to 1800 BC.
Field identification & locations
Identify by its hardness (cannot be scratched by a steel knife) and its smooth, shell-like (conchoidal) fracture surface. Common in the Western United States, Brazil, and India. Look for opaque stones with a waxy feel that occur as nodules or in seams.
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