
metamorphic
Polished green-and-white jasper (likely ocean jasper or orbicular jasper)
Microcrystalline quartz/chalcedony (SiO₂) with chlorite, epidote, calcite, and iron-oxide inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque to slightly translucent, green, cream, and gray mottling; vitreous to waxy luster; cryptocrystalline quartz with no visible cleavage. The elongated specimen is cut and polished, likely shaped as a tower.
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Physical properties
Hardness about 6.5–7 Mohs; opaque to slightly translucent, green, cream, and gray mottling; vitreous to waxy luster; cryptocrystalline quartz with no visible cleavage. The elongated specimen is cut and polished, likely shaped as a tower.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic ash, lava, or sediment, with later alteration producing green chlorite/epidote colors; it is generally Paleozoic to Cenozoic depending on locality. Orbicular varieties develop concentric mineral-growth patterns during alteration.
Uses & applications
Used for ornamental carvings, cabochons, towers, beads, and decorative stone; it has little industrial value compared with ordinary quartz.
Geological facts
Green jasper is often marketed under locality or trade names, and “ocean jasper” is specifically associated with orbicular material from Madagascar; the exact variety cannot be confirmed from the image alone.
Field identification & locations
Identify by its opaque patterned body, glassy/waxy polish, and inability to scratch with a steel knife; it should not fizz with dilute acid unless calcite is abundant. Common sources include Madagascar, India, Brazil, Australia, and the western United States.
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