
Mineral
Quartz with Limonite Staining
Silicon Dioxide (SiO2) with Hydrated Iron Oxide (FeO(OH)·nH2O)
Hardness: 7 (Quartz) and 4-5.5 (Limonite); Color: Grayish-white with yellow-brown staining; Luster: Vitreous to dull; Crystal structure: Trigonal/Amorphous; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 (Quartz) and 4-5
- Color
- Grayish-white with yellow-brown staining
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 (Quartz) and 4-5.5 (Limonite); Color: Grayish-white with yellow-brown staining; Luster: Vitreous to dull; Crystal structure: Trigonal/Amorphous; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed in hydrothermal veins or as a secondary alteration product. Limonite staining occurs when iron-bearing minerals oxidize in the presence of water (weathering).
Uses & applications
Common quartz is used for glassmaking and abrasives. Iron-stained specimens like this are primarily of interest to amateur collectors or as fill material in construction.
Geological facts
Limonite is not a single mineral but a mixture of hydrated iron oxide minerals like goethite. It often 'paints' quartz crystals a golden or rusty color, which collectors sometimes call 'Golden Healer' in metaphysical circles.
Field identification & locations
Identify in the field by checking if the yellow color is a surface coating or internal staining on a hard, glass-like host rock. Commonly found in areas with high iron content and quartz outcroppings.
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