Clear Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: Colorless/Transparent; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Forms in igneous, metamorphic, and sedimentary environments. Typically crystallizes from magma or precipitates from hydrothermal veins. Often found in pegmatites or as a major constituent of granite.
Uses & Applications
Used in electronics (oscillators), optics, glassmaking, construction (as aggregate), jewelry (faceted stones, beads), and for decorative or holistic collecting.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge in response to applied mechanical stress, which is why it is used in watches.
Field Identification & Locations
Identify by its ability to scratch glass, its lack of cleavage, and its characteristic six-sided crystal points (when intact). Commonly found in quartz veins globally.
Identified on: 4/16/2026
Mode: Standard