
mineral
Polished orbicular jasper (likely ocean jasper)
Microcrystalline quartz (SiO₂), chiefly chalcedony with iron oxides and other silicate inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque pale green, cream, and brown banding with a waxy to vitreous polish. Usually massive and non-cleavable, with conchoidal fracture; specific gravity roughly 2.5–2.7.
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Physical properties
Hardness about 6.5–7 Mohs; opaque pale green, cream, and brown banding with a waxy to vitreous polish. Usually massive and non-cleavable, with conchoidal fracture; specific gravity roughly 2.5–2.7.
Formation & geological history
Forms when silica-rich fluids replace or fill cavities in volcanic rock, incorporating iron and other mineral impurities; the attractive orbicular/banded textures developed during alteration. Ocean jasper is chiefly associated with Cenozoic volcanic rocks of Madagascar.
Uses & applications
Used for cabochons, carvings, polished slabs, beads, and decorative objects; modestly valued as a lapidary material.
Geological facts
“Jasper” is a broad trade and geological term for opaque, impurity-rich chalcedony or microcrystalline quartz. The specimen appears cut and polished rather than naturally weathered.
Field identification & locations
Identify by its opaque silica body, hardness, waxy polish, and irregular green-cream-brown bands or orbicules; it should resist scratching by steel. Common sources include Madagascar, India, Brazil, and the western United States.
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