
Mineral
Quartz (likely Clear Quartz or Rock Crystal)
Quartz (SiO2)
Hardness: 7 on Mohs scale. Color: Colorless and transparent (as seen in the image). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (though this small fragment doesn't show a distinct crystal form, general habit in larger pieces is prismatic). Cleavage: None (exhibits conchoidal fracture).…
- Hardness
- 7 on Mohs scale
- Color
- Colorless and transparent (as seen in the image)
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Colorless and transparent (as seen in the image). Luster: Vitreous (glassy). Crystal Structure: Hexagonal (though this small fragment doesn't show a distinct crystal form, general habit in larger pieces is prismatic). Cleavage: None (exhibits conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Quartz is one of the most abundant minerals in the Earth's crust. It forms in a wide range of geological environments. It can crystallize from magma (igneous rocks), precipitate from hydrothermal fluids within veins, or form through diagenesis (sedimentary rocks). Rock crystal, the clear variety, often forms in hydrothermal veins, pegmatites, and geodes. Its geological age varies widely depending on the specific deposit, ranging from Precambrian to Cenozoic.
Uses & applications
Industry: Historically used in early radio and electronics due to its piezoelectric properties (oscillators). Also used as an abrasive. Jewelry: Clear quartz is often cut into cabochons, beads, and faceted stones. It can be carved for decorative items. Construction: As sand, quartz is a primary component of concrete, mortar, and glass. High-purity quartz is used in advanced optics and electronics.
Geological facts
Quartz is the second most abundant mineral in the Earth's continental crust. Pure quartz, colorless and transparent, is called Rock Crystal. Other varieties include Amethyst (purple), Citrine (yellow to orange), Rose Quartz (pink), Smoky Quartz (brown to black), and Onyx/Agate (banded varieties). It's resistant to weathering and is commonly found in river sands.
Field identification & locations
Field Identification: Its hardness (scratches glass), conchoidal fracture (curved, shell-like breaks), and vitreous luster are key identifiers. The clear, colorless nature of this specimen points to 'rock crystal' variety. Common Locations: Found globally in various rock types including igneous (granite, rhyolite), metamorphic (gneiss, schist), and sedimentary (sandstone). Notable sources for crystal specimens include Brazil, Arkansas (USA), and the Alps.
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