
mineral
Quartz with inclusions
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Clear to milky white with reddish-brown hematite/iron inclusions; Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to milky white with reddish-brown hematite/iron inclusions; Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed from hydrothermal solutions or cooling magma in igneous rocks like granite. This specimen shows internal fracturing and mineral staining, typical of geothermal veins.
Uses & applications
Used in gemstone collecting, metaphysical 'healing' crystals, lapidary work for jewelry, and industrial uses in glass manufacturing or electronics due to piezoelectric properties.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Specimens like this one, showing internal veining and reddish iron staining, are often called 'Iron Quartz' or 'Fire Quartz' in collector circles.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), its lack of cleavage, and its vitreous luster. Commonly found in mountainous regions or riverbeds worldwide. This polished piece highlights internal clouds and inclusions.
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