
mineral
Polished agate (likely blue-gray chalcedony)
Microcrystalline quartz, SiO₂; chalcedony, possibly banded agate
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; glossy, waxy luster with translucent blue-gray and white areas. Quartz has a trigonal crystal structure, but its microscopic grains show no visible cleavage; the pictured piece appears tumbled or polished.
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Physical properties
Hardness 6.5–7 Mohs; glossy, waxy luster with translucent blue-gray and white areas. Quartz has a trigonal crystal structure, but its microscopic grains show no visible cleavage; the pictured piece appears tumbled or polished.
Formation & geological history
Silica-rich fluids deposited quartz in cavities, commonly in volcanic rock; agate formed by successive deposition and banding. Its precise age and locality cannot be determined from the image.
Uses & applications
Used for jewelry, beads, and decorative objects; agate is also used in small ornaments and lapidary work.
Geological facts
Agate is a variety of chalcedony, not a separate mineral species; its distinctive bands form as silica layers accumulate over time.
Field identification & locations
Look for translucency, waxy luster, hardness, and natural curved bands; common sources include Brazil, Uruguay, India, and the western United States.
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