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Silicates & Quartz

Quartz

What it is

The most abundant mineral on Earth's surface. Quartz is pure silicon dioxide that crystallizes in hexagonal prisms. Trace impurities and natural radiation create the wide range of colors — iron makes amethyst purple, titanium fibers make rose quartz pink, and aluminum makes smoky quartz brown.

How it forms

Forms in almost every geological environment: igneous pegmatites, hydrothermal veins, metamorphic rocks, and sedimentary deposits. Quartz crystallizes from silica-rich fluids as they cool, typically between 100–500°C. The slower the cooling, the larger the crystals.

SiO₂ — Silicon Dioxide (Hexagonal crystal system)

Specimens

16 stones