
sedimentary
Red Jasper
Silicon Dioxide with Hematite inclusions (SiO2 + Fe2O3)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brick red to brownish-red with dark streaks; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish-red with dark streaks
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to brownish-red with dark streaks; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from volcanic ash or water in sedimentary environments. Hematite impurities provide the red color. Found in environments spanning from Precambrian age to recent eras, often appearing in band formations or as nodules.
Uses & applications
Used primarily for lapidary work, jewelry (beads, cabochons), ornamental vases, and as a popular stone for carving and metaphysical collecting. Historically used for seal stones and tools.
Geological facts
Jasper has been a favorite gemstone since the ancient world, referenced in the Bible and utilized by Ancient Egyptians for amulets. It is an opaque variety of chalcedony.
Field identification & locations
Identify by its rich red color, extreme hardness (not easily scratched by steel), and lack of transparency. It is common in riverbeds and desert environments globally, including India, Brazil, and the USA.
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