
mineral
Small quartz fragment, possibly milky quartz
Quartz (SiO₂)
AI-generated identification · may be incorrectWhite to translucent, vitreous luster, no obvious cleavage, and likely hardness 7 on the Mohs scale; the image is too low-resolution for confident crystal-form identification.
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Physical properties
White to translucent, vitreous luster, no obvious cleavage, and likely hardness 7 on the Mohs scale; the image is too low-resolution for confident crystal-form identification.
Formation & geological history
Quartz commonly crystallizes from silica-rich hydrothermal fluids, igneous melts, and metamorphic veins; individual grains may range from ancient Precambrian material to geologically recent deposits.
Uses & applications
Used in glass, ceramics, abrasives, electronics, and countertops; clear or well-formed crystals are collected and sometimes used as gemstones.
Geological facts
Quartz is one of Earth’s most abundant minerals and is highly resistant to weathering, making it common in stream sediments and sand.
Field identification & locations
Likely quartz if it scratches glass and does not fizz in dilute acid; common worldwide, especially in granite, pegmatite, quartz veins, and quartz-rich sediment. The rounded appearance may indicate tumbling or natural abrasion.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous