sedimentary
Quartz Vein in Host Rock (clastic sediment)
Silicon Dioxide (SiO2) in matrix
Hardness: 7 (quartz) to 5.5 (matrix); Color: White, olive green, tan, grey; Luster: Vitreous to earthy; Crystal Structure: Hexagonal (quartz components); Specific Gravity: ~2.65
- Hardness
- 7 (quartz) to 5
- Color
- White, olive green, tan, grey
- Luster
- Vitreous to earthy
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Physical properties
Hardness: 7 (quartz) to 5.5 (matrix); Color: White, olive green, tan, grey; Luster: Vitreous to earthy; Crystal Structure: Hexagonal (quartz components); Specific Gravity: ~2.65
Formation & geological history
Formed through hydrothermal processes where mineral-rich hot water fills cracks in existing rock, depositing quartz. The outer matrix is a weathered sedimentary stone, likely a siltstone or sandstone, smoothed by water erosion.
Uses & applications
Primarily used as decorative landscaping stone, educational specimens, or as a source of silica in industrial applications if found in large quantities.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specimen shows 'alluvial' wear, meaning its rounded shape was created by the tumbling action of a river or stream over thousands of years.
Field identification & locations
Identify in the field by looking for white crystalline bands cutting through darker, duller rock. Common in stream beds and coastal areas where harder quartz survives erosion better than the surrounding matrix.
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