Quartz Pebble
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: White to milky; Luster: Vitreous to waxy; Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & Geological History
Formed from molten silica cooling in igneous rocks or as veins in metamorphic environments. These specific specimens are river-worn and weathered, likely originating from ancient quartz veins.
Uses & Applications
Used in glassmaking, jewelry (as semi-precious stones), electronics (piezoelectric properties), and commonly as decorative landscaping gravel.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. These milky appearance variations are caused by tiny inclusions of liquid, gas, or both, trapped during crystal growth.
Field Identification & Locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage (it breaks in irregular, shell-like curves). Very common in riverbeds and pebbled beaches.
Identified on: 4/22/2026
Mode: Standard