Gemstones Codexery

Quartz

A hard, abundant mineral used in jewelry and technology.

Quartz

Quartz is a hard mineral composed of silica (silicon dioxide), with atoms linked in a continuous framework of SiO4 tetrahedra. It is the second most common mineral in Earth's lithosphere, comprising about 12% by mass, and has been used since antiquity in jewelry and hardstone carvings, especially in Europe and Asia.

chemical_formula
SiO2
classification
Framework silicate mineral and oxide mineral
hardness
7 on Mohs scale
crystal_system
Trigonal (α-quartz) and hexagonal (β-quartz)
common_varieties
Rock crystal, amethyst, citrine, rose quartz, smoky quartz, milky quartz

Lore & Background

Quartz has been known since antiquity; the Ancient Greeks called it κρύσταλλος (krustallos), meaning 'crystal', believing it to be supercooled ice. Roman naturalist Pliny the Elder also thought quartz was permanently frozen ice, a belief that persisted until the 17th century. In the 17th century, Nicolas Steno's study of quartz established the law of constancy of interfacial angles, paving the way for modern crystallography.

Reader's Guide

Quartz is significant as the defining mineral for hardness 7 on the Mohs scale and as a key component of many rocks, including granite, sandstone, and quartzite. Quartz varieties, from transparent rock crystal to colored amethyst and citrine, have been prized as gemstones for millennia.

Did You Know?

Common Misconceptions (Editorial)

Some people think quartz is rare or only found as clear crystals, but it is actually the second most common mineral in Earth’s lithosphere, comprising about 12% by mass. Others believe the ancient idea that quartz is permanently frozen ice, but this is a misconception—quartz is a hard mineral composed of silica (silicon dioxide), not ice.

Why It Matters (Editorial)

Quartz endures as a subject of fascination not only for its beauty in jewelry and carvings but also for its pivotal role in the history of science. The 17th-century studies of quartz by Nicolas Steno established the law of constancy of interfacial angles, laying the groundwork for modern crystallography, which remains fundamental to geology, chemistry, and materials science.

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