
Mineral
Quartz (likely milky/gray variety)
Quartz (SiO₂)
Hardness: 7 on the Mohs scale. Color: Appears translucent to milky white/gray in the image, often colorless, white, purple (amethyst), pink (rose quartz), yellow (citrine), brown (smoky quartz). Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Appears translucent to milky white/gray in the image, often colorless, white, purple (amethyst), pink (rose quartz), yellow (citrine), brown (smoky quartz). Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Quartz forms in a wide range of geological environments. It can crystallize from magmatic and hydrothermal solutions, making it common in igneous (e.g., granite, rhyolite) and metamorphic rocks (e.g., gneiss, schist, quartzite) as well as hydrothermal veins. Due to its durability, it is also a major component of sedimentary rocks like sandstone. The geological age of quartz varies widely depending on the rock it's part of, spanning billions of years.
Uses & applications
Industry: Used in electronics for oscillators (e.g., watches, radios) due to its piezoelectric properties, in glass making, abrasives, and as a component in ceramics and refractories. Construction: A primary constituent of sand and gravel used in concrete and mortar. Jewelry: Many varieties (amethyst, citrine, rose quartz, smoky quartz, clear quartz) are popular gemstones. Collecting Value: Specimen quality crystals are highly sought after by collectors.
Geological facts
Quartz is one of the most abundant minerals in Earth's continental crust. Its name comes from the German 'Quarz'. It forms the basic component of many rocks and is valued for its piezoelectric and pyroelectric properties. Ancient civilizations used quartz for tools and ornaments, and it has spiritual significance in many cultures.
Field identification & locations
In the field, quartz can often be identified by its glassy luster, hardness (it can scratch glass and steel), and lack of cleavage, resulting in a conchoidal (shell-like) fracture when broken. Its appearance can range from clear to milky to various colors. It's commonly found in nearly all types of geological settings: igneous, metamorphic, and sedimentary rocks, as well as in veins. Tips for collectors include looking for distinct crystal habits in vugs or geodes, or identifying rounded, durable pebbles in riverbeds and beaches.
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