
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Deep brick red to brownish red; Luster: Vitreous to dull; Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Deep brick red to brownish red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Deep brick red to brownish red; Luster: Vitreous to dull; Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water solutions into cavities of volcanic rocks or within sedimentary formations. Its red color comes from iron impurities (hematite) during the lithification process over millions of years.
Uses & applications
Used primarily in lapidary arts for jewelry, decorative carvings, and polished pocket stones. Historically used for ornaments and seals.
Geological facts
Jasper has been a favorite gemstone since antiquity; it is mentioned in the Bible and was highly prized by the ancient Egyptians and Babylonians for its protective qualities.
Field identification & locations
Identify by its opaque nature (unlike carnelian which is translucent) and dull waxy luster before polishing. Commonly found in riverbeds or gravel deposits in India, Russia, Brazil, and the USA (southwestern states).
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