
mineral
Translucent quartz pebble (likely milky quartz)
Quartz, SiO₂; exact variety cannot be confirmed from the photograph
AI-generated identification · may be incorrectWhite to colorless, translucent, with a glassy-to-waxy appearance; hardness 7 Mohs and no cleavage. The uneven, cloudy interior may reflect inclusions or fractures; crystal structure is trigonal.
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Physical properties
White to colorless, translucent, with a glassy-to-waxy appearance; hardness 7 Mohs and no cleavage. The uneven, cloudy interior may reflect inclusions or fractures; crystal structure is trigonal.
Formation & geological history
Quartz commonly forms in hydrothermal veins and igneous or metamorphic rocks, then survives weathering as rounded stream or soil pebbles. Its age cannot be determined visually.
Uses & applications
Quartz is used in glass, ceramics, electronics, and as a collector specimen; this small, rough pebble has little jewelry value unless cut or polished.
Geological facts
The bright glow is transmitted light, not evidence of fluorescence; many quartz pebbles appear luminous when held over a phone light.
Field identification & locations
Look for hardness (it should scratch glass), lack of cleavage, and conchoidal fracture. Quartz is widespread, including in volcanic and metamorphic terrain in central Mexico; the coarse location prior is plausible but not diagnostic.
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