Milky Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Opaque white with iron staining (yellowish-brown); Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.
Formation & Geological History
Formed primarily in hydrothermal veins or as a constituent of igneous rocks like granite. This specific specimen is a water-worn river pebble, likely transported and smoothed by water over long geological periods.
Uses & Applications
Used in construction as aggregate, in glassmaking, as an abrasive, and sometimes in landscaping. High-purity quartz is used in electronics for its piezoelectric properties.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. The white 'milky' color is caused by tiny inclusions of gas or liquid trapped during the crystal's growth.
Field Identification & Locations
Identified by its white color, inability to be scratched by a steel knife, and rounded 'river rock' texture. It is ubiquitous in riverbeds, glacial deposits, and mountain trails worldwide.
Identified on: 5/15/2026
Mode: Standard