
sedimentary
Green Jasper
Microcrystalline Quartz (Chalcedony), SiO2
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale. Color: Muted green, sometimes with banding or inclusions. Luster: Vitreous to waxy. Crystal structure: Trigonal (microcrystalline). Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.58 to 2.91.
- Hardness
- 6
- Color
- Muted green, sometimes with banding or inclusions
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Muted green, sometimes with banding or inclusions. Luster: Vitreous to waxy. Crystal structure: Trigonal (microcrystalline). Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.58 to 2.91.
Formation & geological history
Forms through the precipitation of silica from aqueous solutions, often within silica-rich ash beds or marine sediments, or as a secondary filling in rock fractures. Geological age varies widely depending on the deposit location, spanning from Precambrian to Cenozoic eras.
Uses & applications
Used extensively for ornamental carvings, cabochons in jewelry, spheres, and as a popular specimen for mineral collectors.
Geological facts
Jasper has been used by ancient civilizations for thousands of years to create tools, seals, and decorative ornaments. Green jasper, in particular, was historically prized by the ancient Egyptians and Romans for amulets and signet rings.
Field identification & locations
Easily identified in the field by its conchoidal fracture, waxy luster, opaque nature, and distinct hardness that easily scratches glass. Commonly found in riverbeds, hydrothermal veins, and sedimentary rock formations globally.
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