
mineral
Chalcedony (likely agate)
Microcrystalline quartz, SiO₂; agate is banded chalcedony
AI-generated identification · may be incorrectTranslucent gray with honey-brown edges and a waxy to vitreous luster; hardness about 6.5–7 Mohs, trigonal quartz structure, no cleavage, and conchoidal fracture. The image does not show clear banding, so agate identification is uncertain.
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Physical properties
Translucent gray with honey-brown edges and a waxy to vitreous luster; hardness about 6.5–7 Mohs, trigonal quartz structure, no cleavage, and conchoidal fracture. The image does not show clear banding, so agate identification is uncertain.
Formation & geological history
Silica-rich fluids deposited quartz in cavities and fractures, commonly in volcanic rocks; chalcedony formed across many geological ages and settings.
Uses & applications
Used for carvings, beads, cabochons, ornamental objects, and as a collector specimen.
Geological facts
Chalcedony is quartz made of crystals too small to distinguish unaided; agate is its distinctly banded variety.
Field identification & locations
Look for waxy translucence and curved, shell-like fracture surfaces; agate is typically confirmed by visible bands. Chalcedony occurs worldwide, including Brazil, Uruguay, India, and the western United States.
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