
mineral
Yellow chalcedony (likely honey agate/jasper)
Microcrystalline quartz, SiO₂; may contain iron-oxide inclusions
AI-generated identification · may be incorrectMohs hardness 6.5–7; yellow to orange-brown, waxy to dull luster, cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded, opaque appearance suggests jasper or iron-stained chalcedony rather than gem-quality transparent quartz.
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Physical properties
Mohs hardness 6.5–7; yellow to orange-brown, waxy to dull luster, cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded, opaque appearance suggests jasper or iron-stained chalcedony rather than gem-quality transparent quartz.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures, later colored by iron oxides; commonly Cenozoic to older volcanic or sedimentary host rocks. Exact age cannot be determined from the photograph.
Uses & applications
Used as a lapidary stone for cabochons, beads, carvings, and tumbled stones; attractive pieces are collectible but usually inexpensive.
Geological facts
Chalcedony is quartz composed of extremely small intergrown crystals. Yellow coloration commonly results from hydrated iron oxides or other mineral impurities.
Field identification & locations
Identify by its fine, uniform texture, waxy surface, hardness, and conchoidal fracture; it should not be scratched easily by a steel knife. Common sources include Brazil, Uruguay, Madagascar, India, and the western United States.
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