
sedimentary
Quartz Veined Quartzite or Sandstone
Quartzite with Quartz Veins (SiO2)
Hardness: 7 on the Mohs scale. Color: Brownish-beige with lighter, off-white quartz veins. Luster: Vitreous to dull. Crystal structure: Microcrystalline quartz matrix with macrocrystalline quartz veins. Cleavage: None, fractures conchoidally. Specific gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Brownish-beige with lighter, off-white quartz veins
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 on the Mohs scale. Color: Brownish-beige with lighter, off-white quartz veins. Luster: Vitreous to dull. Crystal structure: Microcrystalline quartz matrix with macrocrystalline quartz veins. Cleavage: None, fractures conchoidally. Specific gravity: 2.65.
Formation & geological history
Formed through the metamorphism of quartz-rich sandstone or through hydrothermal activity where silica-rich fluids filled fractures in pre-existing rock, later subjected to weathering and water transport to form a rounded pebble.
Uses & applications
Used in landscaping, decorative stone, gravel, and as a natural geological specimen for collectors.
Geological facts
The lighter lines running across the stone are quartz veins, which form when hot, mineral-rich fluids circulate through fractures in the rock and deposit crystalline quartz.
Field identification & locations
Easily identified in the field by its extreme hardness (scratches glass), lack of reaction to acid, and distinct contrasting veins. Commonly found in riverbeds and glacial tills.
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Fossiliferous Concretion
Septarian Concretion containing Brachiopods/Crinoids
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Quartz pebble
Silicon dioxide (SiO2)
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Sedimentary Sandstone
Arenite (Sedimentary Rock)
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Generic Pebble / Rock Fragment
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Banded Siltstone / Mudstone Pebble
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