
mineral
Quartz pebble (Chert / Chalcedony)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: brownish-tan, semi-translucent; Luster: waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: none (conchoidal fracture); Specific Gravity: ~2.65
- Hardness
- 7 on Mohs scale
- Color
- brownish-tan, semi-translucent
- Luster
- waxy to vitreous
Identified More mineral →
Explore Quartz pebble (Chert / Chalcedony) 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: brownish-tan, semi-translucent; Luster: waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: none (conchoidal fracture); Specific Gravity: ~2.65
Formation & geological history
Formed via precipitation of silica-rich fluids in sedimentary or volcanic environments, later weathered, rounded, and smoothed by water transport in rivers or ocean shores.
Uses & applications
Commonly collected as river rocks, used in lapidary work, landscape gravel, or tumbled into decorative polished stones.
Geological facts
Water-worn quartz and chert pebbles are among the most durable rocks on Earth, surviving millions of years of erosion due to their high resistance to mechanical and chemical weathering.
Field identification & locations
Identify in the field by its hardness (scratches glass easily), smooth rounded shape, waxy appearance, and translucent light transmission when held to a bright light source. Found in stream beds, beaches, and glacial deposits worldwide.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
mineral
Schist
Schist
Metamorphic
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary