
mineral
Quartz (River Pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Milky white to off-white; Luster: Vitreous to waxy; Structure: Hexagonal/Trigonal; no cleavage; Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to off-white
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to off-white; Luster: Vitreous to waxy; Structure: Hexagonal/Trigonal; no cleavage; Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed through the cooling of magma or precipitation from hydrothermal veins. This specific specimen is a tumbled pebble, meaning it was weathered from its original source and rounded by the abrasive action of water (river or beach) over many years.
Uses & applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, and as decorative landscaping stones or jewelry beads.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These rounded white pebbles are often called 'lucky stones' or 'moon stones' by children though they are geologically common milky quartz.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and steel), its lack of cleavage, and its smooth, rounded 'water-worn' texture. Found globally in riverbeds and coastal regions.
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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