Quartz pebble
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: White/Translucent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed from cooling magma or precipitation in hydrothermal veins. This specific specimen appears to be a water-worn fragment, likely eroded from a larger vein and rounded by transport in water.
Uses & Applications
Source of silica for glassmaking, abrasives, quartz watches (piezoelectric properties), and aggregate in landscaping/construction.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. It is extremely resistant to chemical and physical weathering, which is why it is the primary component of most beach sand.
Field Identification & Locations
Identify in the field by its ability to scratch glass, its lack of cleavage (it breaks into curved shards), and its resistance to acid. Widely found in riverbeds, beaches, and soil globally.
Identified on: 4/21/2026
Mode: Standard