
mineral
Quartz with Mica (Muscovite/Biotite)
Silicon Dioxide (SiO2) with Phyllosilicate inclusions
Hardness: 7 for quartz, 2-2.5 for mica; Color: White/clear quartz with silvery or dark metallic mica flakes; Luster: Vitreous for quartz, pearly to metallic for mica; Crystal structure: Trigonal (quartz), Monoclinic (mica); Specific Gravity: 2.65 for quartz
- Hardness
- 7 for quartz, 2-2
- Color
- White/clear quartz with silvery or dark metallic mica flakes
- Luster
- Vitreous for quartz, pearly to metallic for mica
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Physical properties
Hardness: 7 for quartz, 2-2.5 for mica; Color: White/clear quartz with silvery or dark metallic mica flakes; Luster: Vitreous for quartz, pearly to metallic for mica; Crystal structure: Trigonal (quartz), Monoclinic (mica); Specific Gravity: 2.65 for quartz
Formation & geological history
Formed in pegmatites or hydrothermal veins where silica-rich fluids crystallized alongside sheet silicates deep within the Earth's crust.
Uses & applications
Used in mineral collections, lapidary work, and decorative display.
Geological facts
Quartz is one of the most abundant minerals on Earth, and when found with reflective mica flakes, it is often colloquially mistaken for gold by novice prospectors (hence the nickname 'fool's gold' when pyrite is involved, though mica has its own distinct flaky look).
Field identification & locations
Easily identified by the hard, glassy white quartz matrix contrasting with soft, flexible sheets of reflective mica. Commonly found in pegmatite dykes and metamorphic rocks worldwide.
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