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

Physical Properties
Hardness: 7 on Mohs scale; Color: Milky white with brownish iron staining; Luster: Vitreous to greasy; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed via hydrothermal activity where silica-rich fluids cool in veins or as a major constituent of igneous rocks like granite. This specific specimen has been smoothed and rounded by fluvial (river) or glacial erosion.
Uses & Applications
Industrial use in glassmaking and abrasives; small pebbles are often used as landscaping gravel or decorative aquarium stones.
Geological Facts
The 'milky' appearance is caused by millions of tiny microscopic bubbles of gas or liquid trapped during the crystal's formation. It is one of the most common minerals on Earth's surface.
Field Identification & Locations
Identified in the field by its hardness (it will scratch glass), its white color, and the lack of cleavage planes. Found globally in riverbeds, beaches, and soil.
Identified on: 5/19/2026
Mode: Standard