
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
Hardness: 6.5-7 (Mohs scale); Color: Deep brick red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Deep brick red to brownish-red
- Luster
- Vitreous to dull
Identified More sedimentary →
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Deep brick red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed via the accumulation of silica-rich micro-organisms or volcanic ash within sedimentary environments; the red color comes from iron oxide (hematite) impurities during the mineralization process over millions of years.
Uses & applications
Used primarily in lapidary arts for cabochons, beads, and decorative carvings; historically used for seals, jewelry, and talismans; also popular in metaphysical collections.
Geological facts
Jasper was a favorite gem in the ancient world, referenced in many cultures including Greek and Roman literature; it is considered one of the 'stones of the breastplate' in biblical history.
Field identification & locations
Identify by its opaque nature (it does not transmit light even on thin edges), its characteristic deep red streak, and its high hardness (it will scratch glass). Commonly found in the United States (western states), India, Russia, Brazil, and South Africa.
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