
mineral
Quartz (specifically Milky/Gray Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Grayish-white, translucent; Luster: Vitreous (glassy) to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Grayish-white, translucent
- Luster
- Vitreous (glassy) to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Grayish-white, translucent; Luster: Vitreous (glassy) to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed from the cooling of silica-rich magma or from hydrothermal veins. It is one of the most abundant minerals in the Earth's crust and can be found in rocks from virtually every geological age, often forming in igneous pegmatites or metamorphic environments.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as a component in concrete. In jewelry, it is often tumbled or cut into cabochons; however, common specimens like this are primarily for amateur collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Ancient Greeks named it 'krustallos' meaning ice, as they believed it was permanently frozen water that would never melt.
Field identification & locations
Identify in the field by its hardness (it can scratch steel and glass) and its lack of cleavage (it breaks in irregular, shell-like curves). It is commonly found in riverbeds, mountain scree, and as veins in larger rock outcroppings.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral