
mineral
Polished agate (likely carnelian or orange chalcedony)
Microcrystalline quartz, SiO₂; chalcedony with iron-oxide coloring
AI-generated identification · may be incorrectTranslucent orange, honey-yellow, cream, and brown areas with a waxy-to-glassy luster. Quartz hardness 6.5–7 Mohs; trigonal quartz crystals are microscopic, so no visible cleavage. The photo shows a polished pebble; banding is not clearly visible.
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Physical properties
Translucent orange, honey-yellow, cream, and brown areas with a waxy-to-glassy luster. Quartz hardness 6.5–7 Mohs; trigonal quartz crystals are microscopic, so no visible cleavage. The photo shows a polished pebble; banding is not clearly visible.
Formation & geological history
Silica-rich fluids deposited microcrystalline quartz in cavities or fractures, with iron oxides producing orange tones. Such material forms in many volcanic and sedimentary settings across geologic time.
Uses & applications
Used for beads, cabochons, ornaments, and small carvings; agate is also collected as a polished specimen.
Geological facts
Agate is a variety of chalcedony; the name often describes patterned or banded material, while uniformly orange chalcedony is commonly called carnelian.
Field identification & locations
Identify by its fine-grained, translucent quartz character, hardness, and lack of cleavage; orange color alone cannot confirm agate or carnelian. Chalcedony occurs worldwide, including Brazil, Uruguay, India, and the western United States.
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