
mineral
Orbicular jasper (likely ocean jasper)
Silica-rich microcrystalline quartz/chalcedony with iron-oxide and other mineral inclusions; commonly classified as orbicular jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; gray, brown, cream, and reddish colors with rounded orbicular patterns; opaque, waxy to dull luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture.
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Physical properties
Hardness about 6.5–7 Mohs; gray, brown, cream, and reddish colors with rounded orbicular patterns; opaque, waxy to dull luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture.
Formation & geological history
Forms when silica-rich volcanic or hydrothermal fluids replace or cement rock, while concentric mineral growth creates the orbs. Ocean jasper is especially associated with Miocene volcanic rocks of Madagascar, though similar orbicular jaspers occur elsewhere.
Uses & applications
Used as a lapidary material for cabochons, beads, carvings, polished spheres, and ornamental specimens; rarely used industrially because of its decorative value.
Geological facts
The specimen’s rounded contrasting patches and siliceous appearance strongly suggest orbicular jasper, but a precise variety requires closer inspection or testing.
Field identification & locations
Look for opaque chalcedony, hardness near quartz, conchoidal fracture, and naturally rounded orb patterns; common sources include Madagascar, Mexico, Indonesia, and Oregon. Avoid confusing it with dyed agate or slag.
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