
mineral
Polished brecciated jasper pendant
Jasper, an opaque microcrystalline variety of chalcedony (mostly SiO₂), with iron-oxide staining and likely brecciation
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; orange-red, yellow, brown, and gray mottling; opaque, waxy to vitreous luster after polishing; cryptocrystalline quartz with no visible cleavage. The metal setting and cord are human-made, but the pendant contains genuine geological material.
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Physical properties
Hardness about 6.5–7 Mohs; orange-red, yellow, brown, and gray mottling; opaque, waxy to vitreous luster after polishing; cryptocrystalline quartz with no visible cleavage. The metal setting and cord are human-made, but the pendant contains genuine geological material.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic, sedimentary, or brecciated rock, commonly incorporating iron oxides that produce red, orange, and yellow colors. Its exact geological age and locality cannot be determined from the photograph.
Uses & applications
Used for cabochons, pendants, beads, carvings, and ornamental objects; occasionally as a minor decorative stone in architecture. Its appeal is primarily its pattern and polish rather than rarity.
Geological facts
The colorful patches likely reflect iron minerals such as hematite or goethite; blue-gray areas may be contrasting silica or matrix. Jasper is a variety of chalcedony, not technically a separate mineral species.
Field identification & locations
Identify by its opaque appearance, very fine texture, quartz-like hardness, and inability to scratch with a steel knife easily; it should not show glassy transparency. Common sources include India, Madagascar, Brazil, Australia, Mexico, and the western United States.
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