
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite impurities
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brick red to deep dark red; Luster: Dull to vitreous; Structure: Microcrystalline (Cryptocrystalline) Quartz; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to deep dark red
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to deep dark red; Luster: Dull to vitreous; Structure: Microcrystalline (Cryptocrystalline) Quartz; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed via the deposition of silica from hydrothermal solutions or in sedimentary environments where iron oxides (hematite) provide the red pigment. It is often found in prehistoric iron-rich sedimentary deposits.
Uses & applications
Used extensively for lapidary work, jewelry (cabochons, beads), decorative carvings, and as a popular specimen for rock collectors. Historically used for making stone tools due to its hardness and fracture.
Geological facts
Red jasper has been used since antiquity; it was known as the 'rain bringer' in some cultures and was mentioned in the Bible. It is an opaque variety of chalcedony.
Field identification & locations
Identify by its deep red color and extreme hardness (it will scratch glass). Look for it in river beds or areas with iron-rich soil. It is commonly found in India, Russia, Brazil, and the USA.
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