
sedimentary
Polished rainbow jasper (likely ocean/imperial jasper)
Microcrystalline quartz (SiO₂) with iron oxides and varied silicate inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque, multicolored red, tan, green, cream, and purple bands; waxy to vitreous luster and no visible cleavage. The oval cabochon is polished and likely cut from brecciated or flow-banded jasper.
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Physical properties
Hardness about 6.5–7 Mohs; opaque, multicolored red, tan, green, cream, and purple bands; waxy to vitreous luster and no visible cleavage. The oval cabochon is polished and likely cut from brecciated or flow-banded jasper.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic ash, sediments, or fractured rock; iron and other impurities create the colors. Geological ages vary widely, commonly Precambrian to Cenozoic depending on deposit.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and lapidary collections; generally decorative rather than industrial.
Geological facts
The specimen appears human-cut and polished, so its original texture is enhanced by the cabochon shape and glossy surface. “Rainbow jasper” is a trade name rather than a single precisely defined mineral species.
Field identification & locations
Identify it by its opaque patterned body, hardness, lack of cleavage, and fine-grained quartz texture; it should not fizz in dilute acid. Similar material occurs in Madagascar, Mexico, India, Indonesia, and the western United States.
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