Quartz Pebble

Silicon Dioxide (SiO2)

Rock Type: mineral

Quartz Pebble

Physical Properties

Hardness: 7 on Mohs scale; Color: White to creamy tan; Luster: Vitreous to waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & Geological History

Formed from cooling magma or precipitation in hydrothermal veins. These specific smooth specimens were rounded by alluvial or marine erosion (water action). Age can range from millions to billions of years depending on the source vein.

Uses & Applications

Used in landscaping, construction aggregate, glass making, and as pocket stones for collectors. High-purity quartz is used in electronics and optics.

Geological Facts

Quartz is the second most abundant mineral in Earth's continental crust. These smooth 'river stones' are naturally tumbled by the energy of moving water over long periods.

Field Identification & Locations

Identify by its hardness (cannot be scratched by a steel knife) and lack of cleavage. Found globally in riverbeds, beaches, and gravel pits. Common for beginners to collect due to its durability and tactile smoothness.

Identified on: 4/21/2026

Mode: Standard