
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Creamy white to translucent yellowish; Luster: Vitreous to waxy; Crystal Structure: Trigonal; Cleavage: None; Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Creamy white to translucent yellowish
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Creamy white to translucent yellowish; Luster: Vitreous to waxy; Crystal Structure: Trigonal; Cleavage: None; Specific Gravity: 2.65.
Formation & geological history
Formed from molten silica cooling in igneous rocks or as veins in metamorphic environments. This specific specimen has been rounded and smoothed by water erosion through transport in a river or coastal environment.
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, and as a low-cost decorative garden stone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These small pebbles are often referred to as 'river stones' or 'sea glass' neighbors when found in nature.
Field identification & locations
Identify by its hardness (will scratch glass) and lack of cleavage. Found worldwide in riverbeds, beaches, and gravel pits.
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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