
sedimentary
Jasper with Iron Staining
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Dark green to brownish-yellow/orange (iron staining), Luster: Dull to waxy, Crystal Structure: Microcrystalline (Trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.91
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Dark green to brownish-yellow/orange (iron staining), Luster: Dull to waxy, Crystal Structure: Microcrystalline (Trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or volcanic ash into sedimentary environments. The specific coloration suggests iron oxide infiltration during or after formation. Most jasper dates from the Precambrian to present times.
Uses & applications
Commonly used in jewelry (cabochons, beads), decorative lapidary arts, and stone healing practices. In some contexts, it is processed for decorative aquarium or landscaping gravel.
Geological facts
Jasper is a variety of chalcedony that is opaque due to high mineral impurities. The word Jasper comes from the Greek word 'iaspis', meaning 'spotted stone.' It has been a favored gemstone since antiquity, mentioned in ancient literature and used for seals in Crete.
Field identification & locations
Identify in the field by its hardness (it should scratch glass), opaque nature, and waxy luster when freshly broken. Commonly found in riverbeds or desert regions globally, especially in Oregon, California, and India. Collectors look for unique banding patterns.
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