Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale), Color: Colorless/Transparent, Luster: Vitreous (glassy), Crystal system: Hexagonal/Trigonal, Cleavage: None/Conchoidal fracture, Specific gravity: 2.65
Formation & Geological History
Forms in all types of environments (igneous, metamorphic, and sedimentary) through crystallization of silica-rich molten rock or hydrothermal veins. Found in formations of all geological ages.
Uses & Applications
Used in electronics (oscillators), manufacturing of glass and ceramics, jewelry (gemstones), and as decorative collector specimens.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is traditionally called rock crystal or clear quartz and is often found in clusters of hexagonal prisms.
Field Identification & Locations
Identify by its six-sided prismatic habit, hardness (will scratch glass), and lack of cleavage. Commonly found in mountainous regions worldwide, including Arkansas (USA), Brazil, and the Alps.
Identified on: 4/27/2026
Mode: Standard