
mineral
Black-and-white agate geode pendant
Agate (microcrystalline quartz, SiO₂), likely a hollow geode slice with chalcedony and drusy quartz
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; waxy to vitreous luster, concentric banding, black/gray chalcedony, and a pale crystalline cavity. Quartz is trigonal, with no cleavage; the rim appears gold-plated and human-made.
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Physical properties
Hardness 6.5–7 Mohs; waxy to vitreous luster, concentric banding, black/gray chalcedony, and a pale crystalline cavity. Quartz is trigonal, with no cleavage; the rim appears gold-plated and human-made.
Formation & geological history
Forms when silica-rich groundwater fills cavities in volcanic rock, depositing layered chalcedony and later quartz crystals. Agate formation commonly occurred from the Paleozoic through Cenozoic eras, depending on locality.
Uses & applications
Used for pendants, cabochons, carvings, ornaments, and lapidary pieces; this example is jewelry-grade mainly for its contrasting banding and geode cavity.
Geological facts
Agate’s bands often record successive changes in groundwater chemistry. Black coloration may be natural manganese/iron-related material or enhancement, and the metal setting is not geological.
Field identification & locations
Identify by translucent chalcedony, curved banding, conchoidal fracture, and hardness sufficient to scratch glass; avoid confusing it with dyed glass or resin. Common sources include Brazil, Uruguay, Mexico, India, and Madagascar.
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