
mineral
Tumbled chalcedony or quartzite pebble
Microcrystalline quartz, SiO₂ (likely chalcedony; exact identification requires testing)
AI-generated identification · may be incorrectPale lavender-gray to cream, opaque to slightly translucent, with a smooth water-worn/tumbled surface and dull-to-waxy luster. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.
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Physical properties
Pale lavender-gray to cream, opaque to slightly translucent, with a smooth water-worn/tumbled surface and dull-to-waxy luster. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.6.
Formation & geological history
Likely formed as silica-rich material in a volcanic or sedimentary environment, then rounded naturally or by tumbling; its precise geological age and source cannot be determined from the image.
Uses & applications
Used for lapidary cabochons, beads, carvings, and decorative stones; common pieces have limited jewelry value.
Geological facts
The lavender tint may reflect trace iron, manganese, or other impurities, but color alone cannot confirm amethyst. A steel blade should not scratch quartz, while quartz should scratch ordinary glass.
Field identification & locations
Common as rounded stream, beach, or landscaping pebbles worldwide, especially in quartz-rich terrains. Confirm with hardness, a glass-scratch test, translucency, and specific-gravity testing; acid testing is generally uninformative.
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