Quartz on Schist
Silicon Dioxide (SiO2) on Foliated Metamorphic Rock
Rock Type: metamorphic

Physical Properties
Hardness: 7 (Quartz) / 3-4 (Schist matrix); Color: Milky white to clear quartz on gray/silvery matrix; Luster: Vitreous to pearly; Crystal structure: Trigonal (Quartz); cleavage: None in quartz, perfect basal in schist mica.
Formation & Geological History
Formed through regional metamorphism of clay-rich sedimentary rocks (shale) under high pressure and temperature. The quartz veins typically precipitate from hydrothermal fluids filling fractures during the later stages of metamorphism.
Uses & Applications
Primarily used for geological study, teaching specimens, and as a common decorative rock for amateur collectors. Quartz is used in electronics and glass, while schist has limited use as decorative stone.
Geological Facts
Schist is characterized by its high mica content, which gives it a distinct 'shimmer.' The presence of quartz veins often highlights the tectonic stress the rock underwent during formation.
Field Identification & Locations
Identify by looking for 'platy' or flaky mineral layers (schistosity) and testing the hard, glass-like white mineral for scratch resistance against steel. Commonly found in mountain ranges and metamorphic belts worldwide.
Identified on: 5/12/2026
Mode: Standard