
sedimentary
Jasper (Iron-stained)
Silicon Dioxide (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Dark green to black with yellow/brown iron veins; Luster: Waxy to dull (tumble-smooth); Crystal structure: Microcrystalline/Cryptocrystalline hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.9
- Hardness
- 6
- Color
- Dark green to black with yellow/brown iron veins
- Luster
- Waxy to dull (tumble-smooth)
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Dark green to black with yellow/brown iron veins; Luster: Waxy to dull (tumble-smooth); Crystal structure: Microcrystalline/Cryptocrystalline hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.9
Formation & geological history
Formed from the deposition of silica from water solutions into cracks or cavities in other rocks, or within volcanic ash beds. The colors come from iron and other mineral impurities present during the sedimentary process over millions of years.
Uses & applications
Commonly used for lapidary work, jewelry (cabochons), or as decorative 'pocket stones' and tumbled collectibles.
Geological facts
Jasper is an opaque variety of chalcedony. It has been used for ornamentation and tools since the Neolithic period. The specific specimen shown is a water-worn or tumbled cobble with distinct quartz/iron mineral veins.
Field identification & locations
Identify in the field by its smoothness (if found in rivers), lack of visible grains, and extreme hardness (it will scratch glass). Often found in riverbeds, glacial deposits, and coastal beaches.
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