
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: White to translucent milky white, Luster: Vitreous (glassy) to waxy when water-worn, Crystal structure: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65.
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Physical properties
Hardness: 7 (Mohs scale), Color: White to translucent milky white, Luster: Vitreous (glassy) to waxy when water-worn, Crystal structure: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal veins or within igneous and metamorphic rocks. This specific specimen has been shaped and polished into a 'sea bean' or pebble through high-energy wave action (abrasion) in a coastal or river environment.
Uses & applications
Industrial use for glass making, abrasives, and electronics (as silicon). Smooth pebbles are used in landscaping, aromatherapy stones, and as 'worry stones' for collectors.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. It is highly resistant to chemical and physical weathering, which is why it often remains as rounded pebbles on beaches long after other minerals have eroded away.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and metal) and lack of cleavage. It often appears milky or 'frosted' on beaches. Common globally in beach shingle and river beds.
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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
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