
mineral
Tumbled Clear Quartz and Citrine Points
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Colorless to yellow/orange, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Colorless to yellow/orange, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed through hydrothermal crystallization in igneous veins or as deposits from silica-rich groundwater. These specimens are often found in pegmatites and geodic cavities.
Uses & applications
Used widely in lapidary work for jewelry, meditation, and healing practice collections. Industrially used in optics and electronics (though usually synthetic for these purposes).
Geological facts
Quartz is the second most abundant mineral in Earth's crust. Citrine is the rare yellow/orange variety of quartz, though most commercial citrine is actually heat-treated amethyst.
Field identification & locations
Identify by its ability to scratch glass, its lack of cleavage, and the presence of six-sided crystal habits. Found globally with major deposits in Brazil and Madagascar.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous