Quartz Pebble
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: White to milky translucent; Luster: Vitreous/Waxy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & Geological History
Formed from the crystallization of silica-rich hydrothermal fluids or within igneous veins. This specific specimen has been rounded and smoothed by fluvial or marine attrition (water erosion over thousands of years).
Uses & Applications
Used primarily for decorative landscaping, gravel, industrial glass production, and occasionally as a source of silicon for electronics.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. White 'milky' quartz gets its color from tiny microscopic inclusions of gas or liquid trapped during the crystal's growth.
Field Identification & Locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and smooth, water-worn surface. Commonly found in riverbeds, beaches, and glacial till worldwide.
Identified on: 4/13/2026
Mode: Standard