
mineral
Milky quartz pebble
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectHardness 7 Mohs; translucent white to pale gray, with a vitreous-to-waxy luster and irregular fracture. It has a trigonal crystal structure, lacks cleavage, and typically has a specific gravity near 2.65.
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Physical properties
Hardness 7 Mohs; translucent white to pale gray, with a vitreous-to-waxy luster and irregular fracture. It has a trigonal crystal structure, lacks cleavage, and typically has a specific gravity near 2.65.
Formation & geological history
Forms when silica-rich fluids crystallize in veins, cavities, and igneous rocks; the cloudy appearance results from microscopic fluid inclusions or fractures. Quartz is common from Precambrian to modern geological settings.
Uses & applications
Used for glass, ceramics, abrasives, electronics, and engineered stone; attractive pieces may be used as inexpensive lapidary material or specimens.
Geological facts
Quartz is one of Earth’s most abundant minerals and is piezoelectric. This small rounded specimen appears naturally weathered or tumbled, though its exact identification cannot be confirmed from the image alone.
Field identification & locations
Identify by its glassy appearance, lack of cleavage, conchoidal fracture, and resistance to scratching; it should scratch ordinary glass but not be scratched by a steel knife. Common worldwide in stream gravels, veins, and quartz-rich rocks.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary