
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Off-white, yellowish-tan, grey with iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Off-white, yellowish-tan, grey with iron staining
- Luster
- Vitreous to greasy
Identified More mineral →
Explore Quartz Pebble in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 on Mohs scale; Color: Off-white, yellowish-tan, grey with iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through weathering and erosion of quartz-bearing rocks such as granite or pegmatites. The rounded shape indicates transport and tumbling by river, stream, or beach wave action over time.
Uses & applications
Commonly used as decorative gravel, in land scaping, aggregate in concrete, or collected as a simple beach/river pebble.
Geological facts
Quartz is one of the most abundant minerals on Earth's surface and is highly resistant to both chemical weathering and physical abrasion, which is why quartz pebbles dominate riverbeds and gravel beaches worldwide.
Field identification & locations
Can be identified by its hardness (scratches glass), lack of cleavage, translucent appearance, and rounded water-worn shape. Found in streams, rivers, beaches, and glacial till across the globe.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock