Clear Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Colorless to white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed through the cooling of silica-rich magma or from hydrothermal veins. It can be found in all types of rocks (igneous, metamorphic, and sedimentary) across almost all geological ages.
Uses & Applications
Used in electronics (oscillators), glassmaking, abrasives, gemstone jewelry, and decorative carvings. It is also highly valued in the metaphysical and collecting communities.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz', and the ancient Greeks believed it was ice that had frozen so hard it would never melt.
Field Identification & Locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and characteristic hexagonal crystal habit if intact. Found globally, especially in mountain ranges like the Alps or the Arkansas Ozarks.
Identified on: 4/17/2026
Mode: Standard