
metamorphic
Quartzite pebble
Quartzite
AI-generated identification · may be incorrectHardness: ~7 on Mohs scale; Color: tan, grey, pinkish, or whitish; Luster: vitreous to grainy; Crystal structure: massive, granular; Cleavage: none, conchoidal fracture
- Hardness
- ~7 on Mohs scale
- Color
- tan, grey, pinkish, or whitish
- Luster
- vitreous to grainy
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Physical properties
Hardness: ~7 on Mohs scale; Color: tan, grey, pinkish, or whitish; Luster: vitreous to grainy; Crystal structure: massive, granular; Cleavage: none, conchoidal fracture
Formation & geological history
Formed through metamorphism of quartz-rich sandstone, where heat and pressure cause the quartz grains to recrystallize and fuse together. Often found in riverbeds or beaches where they have been smoothed by water action over time.
Uses & applications
Used in construction, as decorative stone, and in some industrial applications due to its hardness and durability. Small pebbles are often collected or used in landscaping.
Geological facts
Quartzite is so tough that it often breaks across the quartz grains rather than around them. The pinkish hue in some pebbles comes from trace amounts of iron oxide.
Field identification & locations
Identified by its sugary texture and hardness (it will scratch glass). Commonly found in alluvial deposits, river rocks, and glacial till.
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