
sedimentary
River Cobble (Sandstone)
Arenite / Quartz Sandstone
Hardness: 6-7 (Mohs scale); Color: Gray, tan, and brownish; Luster: Dull/Earthy; Texture: Fine to medium grained with a gritty feel; Crystal structure: Clastic (composed of cemented sand grains); Cleavage: None
- Hardness
- 6-7 (Mohs scale)
- Color
- Gray, tan, and brownish
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs scale); Color: Gray, tan, and brownish; Luster: Dull/Earthy; Texture: Fine to medium grained with a gritty feel; Crystal structure: Clastic (composed of cemented sand grains); Cleavage: None
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral particles or rock fragments. This specific rounded shape is the result of long-term fluvial erosion (river action), which smoothed the edges during transport over many years.
Uses & applications
Commonly used in landscaping, as aggregate in construction, or as decorative stones in gardens and aquariums. Hand-sized smooth stones are also popular for rock painting.
Geological facts
Sandstone makes up about 20% to 25% of all sedimentary rocks on Earth. The rounded edges, or 'well-rounded' texture, indicate that the stone traveled a long distance from its original source before being collected.
Field identification & locations
Identify in the field by its gritty, sandpaper-like texture and rounded, water-worn exterior. It is commonly found in riverbeds, glacial tills, and coastal areas throughout the world.
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