
mineral
Tumbled blue chalcedony, possibly dyed agate
Microcrystalline quartz, SiO₂ (chalcedony)
AI-generated identification · may be incorrectPale blue, polished, translucent to opaque with a waxy-to-glassy luster; quartz crystal structure is too fine-grained to see. Hardness is about 6.5–7 Mohs; the image is too blurry to confirm banding or dye.
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Physical properties
Pale blue, polished, translucent to opaque with a waxy-to-glassy luster; quartz crystal structure is too fine-grained to see. Hardness is about 6.5–7 Mohs; the image is too blurry to confirm banding or dye.
Formation & geological history
Silica-rich groundwater deposits chalcedony in cavities and fractures, often in volcanic rocks; formation may span many geological ages. Tumbling and possible coloring are human processing.
Uses & applications
Used for inexpensive jewelry, ornaments, and lapidary pieces; value depends on material quality and treatment.
Geological facts
Blue chalcedony is commonly colored naturally by trace elements, but vivid or unusually uniform color can indicate dye.
Field identification & locations
Look for a smooth, waxy surface and translucence at thin edges; agate varieties often show bands. Common sources include Brazil, Uruguay, India, and the United States.
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