
Mineral
Quartz
Quartz (SiO₂)
Hardness: 7 on Mohs scale; Color: Colorless, white, purple (amethyst), pink (rose quartz), brown/black (smoky quartz), yellow (citrine); Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless, white, purple (amethyst), pink (rose quartz), brown/black (smoky quartz), yellow (citrine); Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Quartz typically forms from the slow crystallization of silica-rich molten rock (magma or lava) in igneous rocks (e.g., granite, rhyolite). It can also form from hydrothermal solutions in veins, in metamorphic rocks through recrystallization, and as clastic grains in sedimentary rocks from the weathering of pre-existing rocks. Its geological age varies widely depending on the formation process, ranging from billions of years old in ancient cratons to relatively recent formation in active hydrothermal systems.
Uses & applications
Industry: Electronics (oscillators, filters, frequency control), glass manufacturing, abrasives, ceramics, optical instruments. Jewelry: Many varieties are used as gemstones (e.g., amethyst, citrine, rose quartz, smoky quartz, rock crystal). Construction: Sandstone (composed of quartz grains) is used as a building material; quartz sand is used in concrete and mortar.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. It is a major component of many rocks and is found in a wide variety of geological environments. Different color varieties are often given their own names (e.g., Amethyst, Citrine, Rose Quartz, Smoky Quartz). Its piezoelectric properties make it valuable in electronics.
Field identification & locations
Field Identification: Its hardness (scratches glass), conchoidal fracture (smooth, curved breaks), vitreous luster, and common hexagonal crystal habit (though often found anhedral or massive) are key. Common Locations: Found globally in various rock types, including igneous rocks (granite, pegmatites), metamorphic rocks (gneiss, schist, quartzite), and sedimentary rocks (sandstone, chert). Tips for Collectors: Look for well-formed crystals in vugs or veins within igneous and metamorphic rocks. Riverbeds and alluvial deposits can yield water-worn quartz pebbles and crystals. Different color varieties are sought after.
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