
sedimentary
Quartz-veined Sedimentary Rock
Hydrothermally veined Clastic Sedimentary Rock (SiO2 veins in Matrix)
AI-generated identification · may be incorrectHardness: Matrix 3-6 / Veins 7 (Mohs); Color: Tan/grey matrix with white veins; Luster: Dull to vitreous; Crystal structure: Microcrystalline; Cleavage: None/Conchoidal in veins; Specific gravity: ~2.65
- Hardness
- Matrix 3-6 / Veins 7 (Mohs)
- Color
- Tan/grey matrix with white veins
- Luster
- Dull to vitreous
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Physical properties
Hardness: Matrix 3-6 / Veins 7 (Mohs); Color: Tan/grey matrix with white veins; Luster: Dull to vitreous; Crystal structure: Microcrystalline; Cleavage: None/Conchoidal in veins; Specific gravity: ~2.65
Formation & geological history
Formed through the accumulation of mineral particles or rock fragments (matrix), later fractured by tectonic stress. Hot, mineral-rich hydrothermal fluids then filled these cracks, precipitating silica to form white quartz veins.
Uses & applications
Primarily used as aggregate in construction, road base, and decorative landscaping. Some specimens are used in lapidary work as 'wishing stones'.
Geological facts
The appearance of a continuous line or 'belt' around a stone has led to cultural myths, such as 'wishing stones' where a circle of quartz is said to grant luck. These veins are geological records of the rock's stress history.
Field identification & locations
Identify by looking for distinct, protruding white lines (veins) that are harder than the surrounding host rock. Commonly found in riverbeds, glacial tills, and coastal beaches where water has polished the exterior.
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