
sedimentary
Sandstone Pebble
Sandstone (Silicon dioxide-rich clastic sedimentary rock)
AI-generated identification · may be incorrectHardness: 6-7 on Mohs scale depending on cementation; Color: Light brown to grayish-tan; Luster: Dull, earthy; Texture: Granular, fine-to-medium-grained quartz sand matrix; Structure: Rounded beach/river pebble due to fluid erosion.
- Hardness
- 6-7 on Mohs scale depending on cementation
- Color
- Light brown to grayish-tan
- Luster
- Dull, earthy
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Physical properties
Hardness: 6-7 on Mohs scale depending on cementation; Color: Light brown to grayish-tan; Luster: Dull, earthy; Texture: Granular, fine-to-medium-grained quartz sand matrix; Structure: Rounded beach/river pebble due to fluid erosion.
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments (predominantly quartz and feldspar) in marine, fluvial, or desert environments, followed by physical weathering and transport by water.
Uses & applications
Commonly used as construction aggregate, decorative landscaping rock, and for educational stone identification. Smooth pebbles are also popular in rock tumbling and crafts.
Geological facts
River and beach pebbles undergo thousands of years of natural friction and water action, which rounds off their sharp edges to create smooth, oval cobbles. Sandstone accounts for about 20% of all sedimentary rocks on Earth.
Field identification & locations
Identified in the field by its gritty, sandpaper-like texture when rubbed, along with visible tiny quartz grains. Widely abundant in riverbeds, glacial deposits, and coastal beaches around the world.
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