
sedimentary
Jasper (Red Jasper)
Silicon Dioxide (SiO₂)
Hardness: 6.5-7 Mohs scale; Color: Red, brown, earthy tones; Luster: Dull to vitreous; Crystal Structure: Microcrystalline/cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91.
- Hardness
- 6
- Color
- Red, brown, earthy tones
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 Mohs scale; Color: Red, brown, earthy tones; Luster: Dull to vitreous; Crystal Structure: Microcrystalline/cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91.
Formation & geological history
Formed from the deposition of silica from volcanic ash or water circulation through sedimentary rocks. The red color is caused by the inclusion of iron oxide (hematite). It can be found in rocks of various ages ranging from Precambrian to recent times.
Uses & applications
Commonly used in lapidary arts for jewelry, ornaments, seal stones, and as a decorative stone in mosaics and furniture. Historically used to create sharp tools and arrowheads.
Geological facts
Jasper was a favorite gem in the ancient world; its name can be traced back in Hebrew, Assyrian, Greek, and Latin. It is considered one of the traditional birthstones for March.
Field identification & locations
Identify by its opaque nature (unlike agate which is translucent), its smooth conchoidal fracture, and its inability to be scratched by a steel knife. Frequently found in riverbeds, deserts, and volcanic regions globally.
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