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Bruno Balestrini/ Mineralogy/ Black Quartz
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Oxides and Hydroxides

Black Quartz

Quartz is one of the most widespread minerals and the one with the most varieties. These are divided into two main groups, depending on whether they are minerals with clearly visible crystals or minerals formed by aggregates of microscopic crystals. The first group includes pure quartz (hyaline quartz or rock crystal), colourless and transparent, amethyst quartz, smoky quartz or morion, citrine quartz, blue quartz, iris quartz and rose quartz, varieties coloured by impurities. The second group, on the other hand, includes chalcedony (which in turn comprises carnelian, agate and onyx), jasper and flint.

It forms hexagonal prisms, it is stubby or slender, with pyramidal terminations. Quartz is a hard mineral, light, it is not fusible, it is insoluble, except in hydrofluoric acid.

It forms in igneous rocks, metamorphic and sedimentary, and is also frequent in veins of metallic minerals.

Quartz is used in many sectors: domestic (detergents and toothpastes), industrial (glassworks), gemmological for the finest specimens, and also technological (oscillators, ultrasound generators).

This English text was translated with the help of artificial intelligence (Claude) from the Italian original, except where an English version already existed in the original archive. Read the Italian version.