
sedimentary
Polished orbicular jasper (likely kambaba jasper)
Kambaba jasper; cryptocrystalline quartz/chalcedony with dark green and gray orbicular aggregates, commonly associated with altered volcanic material
AI-generated identification · may be incorrectMohs hardness about 6.5–7; dark green-gray, opaque, with pale gray orbicular or brecciated patches and a smooth polished surface; dull to waxy luster; no visible cleavage; specific gravity roughly 2.5–2.7.
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Physical properties
Mohs hardness about 6.5–7; dark green-gray, opaque, with pale gray orbicular or brecciated patches and a smooth polished surface; dull to waxy luster; no visible cleavage; specific gravity roughly 2.5–2.7.
Formation & geological history
Formed from silica-rich, altered volcanic or sedimentary material later silicified and patterned by mineral aggregates; commonly Precambrian in age, though exact age depends on locality.
Uses & applications
Used for cabochons, beads, carvings, palm stones, and lapidary collectibles; generally not used as a construction stone.
Geological facts
Its rounded pale markings can resemble fossil or microbial textures, but many specimens sold as kambaba jasper are geologically variable and may be sold under trade names such as kabamba stone.
Field identification & locations
Identify by the opaque dark green body, rounded gray-green patches, and waxy polish; verify with a hardness or specific-gravity test because serpentine, rhyolite, and other jaspers can look similar. Commonly marketed from Madagascar and parts of Africa.
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