Quartz Pebble
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: White, tan, or milky; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & Geological History
Formed from the crystallization of silica-rich fluids in veins or igneous environments. These specific specimens are water-worn, having been smoothed by mechanical weathering in a riverbed or coastal environment.
Uses & Applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as construction aggregate. Smooth pebbles are commonly used in landscaping and aquarium decor.
Geological Facts
Quartz is the most abundant mineral in the Earth's continental crust. These rounded shapes indicate the rocks have traveled long distances from their source, losing sharp edges through abrasion.
Field Identification & Locations
Identify by its hardness (cannot be scratched by a steel knife) and lack of cleavage. Look for the translucent look and smooth, rounded water-worn texture in stream beds or glacial till.
Identified on: 4/15/2026
Mode: Standard