
mineral
Polished jasper
Microcrystalline quartz (SiO₂), commonly iron-oxide-rich
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque mustard-brown with gray-white bands, earthy to vitreous luster, and no visible crystal faces. It is a polished cabochon/tumbled piece, likely showing chalcedonic quartz and iron-oxide inclusions.
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Physical properties
Hardness about 6.5–7 Mohs; opaque mustard-brown with gray-white bands, earthy to vitreous luster, and no visible crystal faces. It is a polished cabochon/tumbled piece, likely showing chalcedonic quartz and iron-oxide inclusions.
Formation & geological history
Jasper forms when silica-rich groundwater replaces or fills volcanic and sedimentary material, with iron producing yellow-brown coloration. Formation ages vary widely, from Precambrian to younger volcanic settings.
Uses & applications
Used for cabochons, beads, carvings, and ornamental objects; it has modest jewelry and collector value.
Geological facts
The specimen’s broad opaque color fields and irregular banding are typical of jasper rather than transparent agate. Exact variety or locality cannot be determined reliably from the photograph alone.
Field identification & locations
Identify it by its opaque patterned appearance, glassy polish, and resistance to scratching; a steel file should not readily scratch it. Common sources include India, Madagascar, Brazil, Australia, and the western United States.
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