
sedimentary
Red Jasper
Silicon Dioxide (SiO₂)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brick red to deep brownish-red; Luster: Vitreous to dull; Crystal Structure: Hexagonal (Trigonal) microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to deep brownish-red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to deep brownish-red; Luster: Vitreous to dull; Crystal Structure: Hexagonal (Trigonal) microcrystalline quartz; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed from the deposition of silica-rich fluids in sedimentary or low-grade metamorphic environments. Its red color is derived from iron (hematite) inclusions within the cryptocrystalline quartz structure.
Uses & applications
Used primarily in lapidary arts for jewelry, decorative carvings, and cabochons. Historically used for making stone tools and seals. Also popular in metaphysical and crystal collecting markets.
Geological facts
Jasper has been a precious stone since ancient times; it is mentioned in the Bible and was highly valued by the Egyptians and Cretans. The term 'Jasper' is derived from the Greek word 'iaspis', meaning spotted stone.
Field identification & locations
Identify by its opaque nature (unlike translucent carnelian), its high hardness (it will scratch glass), and its smooth, waxy surface when polished. Commonly found in riverbeds or desert regions globally, particularly in India, Brazil, and the USA.
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