
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: White/Milky to translucent, Luster: Vitreous to dull, Crystal Structure: Hexagonal (though not visible in tumbled form), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: White/Milky to translucent, Luster: Vitreous to dull, Crystal Structure: Hexagonal (though not visible in tumbled form), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of magma or precipitation from hydrothermal veins. This specifically is a water-worn pebble, shaped by erosion in a river or coastal environment over thousands of years.
Uses & applications
Commonly used in landscaping, construction aggregate, and glass manufacturing. High-purity quartz is used in electronics and watches. Pebbles like this are often kept as pocket stones or used in aquariums.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz', which means 'hard'. Clear varieties have been used in various cultures as 'healing stones' throughout history.
Field identification & locations
Identify by its hardness (it can scratch glass and steel) and lack of cleavage. Commonly found on beaches, riverbeds, and in gravel pits worldwide. Collectors look for unique shapes or clarity.
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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