
mineral
Quartz (Druzy or Crystalline)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Clear to milky white
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich hydrothermal fluids in rock cavities or veins. It can occur in nearly all geological ages and environments, often crystallizing as the last stage of igneous cooling or within sedimentary geodes.
Uses & applications
Used in watchmaking (quartz movement), electronics (piezoelectric properties), glass manufacturing, abrasives, and as a popular gemstone for jewelry and metaphysical collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. 'Druzy' refers specifically to the tiny glittering crystals that form on the surface of another stone.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and hexagonal crystal shapes. Found globally, especially in mountain ranges and volcanic areas like Brazil, Arkansas (USA), and the Alps.
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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
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock