Quartz Crystal with Inclusions
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: Colorless/transparent with dark brown/black inclusions; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & Geological History
Formed through hydrothermal processes where silica-rich fluids cooled and crystallized in veins or cavities. This specimen shows inclusions of other minerals (likely iron oxides like hematite or goethite) trapped during growth.
Uses & Applications
Used primarily for crystal collecting, metaphysical purposes, and jewelry. Industrial clear quartz is used in electronics and optics due to piezoelectric properties.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Specimens like this one, with visible phantom growths or internal inclusions, are highly prized by collectors as time capsules of geological history.
Field Identification & Locations
Identify by its hardness (scratches glass), glass-like luster, and lack of true cleavage planes. Often found in pegmatites, hydrothermal veins, and sedimentary river beds.
Identified on: 4/23/2026
Mode: Standard