
mineral
Quartz Crystal Cluster with Iron Stain
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, clear to translucent or milky white with orange-brown iron oxide (limonite/hematite) staining, vitreous luster, hexagonal crystal system, conchoidal fracture, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, clear to translucent or milky white with orange-brown iron oxide (limonite/hematite) staining, vitreous luster, hexagonal crystal system, conchoidal fracture, specific gravity of 2.65.
Formation & geological history
Formed from hydrothermal solutions rich in silica within cavities of host rocks, often in pegmatites or veins, over millions of years.
Uses & applications
Used in electronics, watchmaking, glassware, optics, decorative objects, and crystal specimen collecting.
Geological facts
Quartz is one of the most abundant minerals in Earth's continental crust. The reddish-orange staining is typically caused by iron-rich water weathering the crystal surfaces over time.
Field identification & locations
Easily identified by its crystal shape, high hardness (scratches glass), and lack of cleavage. Found worldwide, commonly in pegmatites, hydrothermal veins, and sedimentary deposits.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Granite, a coarse-grained felsic intrusive igneous rock
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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