Quartz Vein in Host Rock
Silicon Dioxide (SiO2) within Metasedimentary or Igneous matrix
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs); Color: Milky white to translucent quartz in a grey/green matrix; Luster: Vitreous to waxy; Structure: Hexagonal; Cleavage: None (conchoidal fracture).
Formation & Geological History
Formed through hydrothermal precipitation where mineral-rich hot water flows through fractures in pre-existing rock, cooling and depositing silica over time.
Uses & Applications
Quartz is used in glassmaking, electronics (piezoelectric properties), abrasives, and as decorative architectural stone or collector specimens.
Geological Facts
Quartz is the most abundant and diverse mineral on Earth's surface. Hydrothermal veins like these are often the primary source for gold and other precious metals.
Field Identification & Locations
Identify in the field by the white 'seam' cutting through darker rock; it will scratch glass and lacks cleavage. Commonly found in mountainous regions or areas with historical tectonic activity.
Identified on: 5/2/2026
Mode: Standard