Clear Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Colorless to transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & Geological History
Formed in a wide range of environments, primarily through the cooling of silica-rich magma or from hydrothermal vents. It is one of the most abundant minerals in the Earth's crust, found in igneous, metamorphic, and sedimentary rocks.
Uses & Applications
Used in electronics (as a piezoelectric material), glassmaking, abrasive blasting, and as a gemstone for jewelry and ornamental carving.
Geological Facts
Clear Quartz is often called Rock Crystal. For centuries, it was believed to be permanently frozen ice because of its transparency and coolness to the touch.
Field Identification & Locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and hexagonal crystal habits. Commonly found in mountainous regions, riverbeds, and as part of granite outcrops.
Identified on: 5/2/2026
Mode: Standard