
sedimentary
Sandstone (specifically Banded Sandstone)
Clastic sedimentary rock (primarily SiO2)
Hardness: 6-7 on Mohs scale; Color: Tan, reddish-pink, or light brown with distinct banding; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific Gravity: 2.2–2.8.
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, reddish-pink, or light brown with distinct banding
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, reddish-pink, or light brown with distinct banding; Luster: Dull/Earthy; Crystal structure: Clastic (grainy); Cleavage: None; Specific Gravity: 2.2–2.8.
Formation & geological history
Formed from the accumulation and cementation of mineral particles or rock fragments, typically sand-sized quartz. The banding (Liesegang rings) often results from the precipitation of iron oxides and hydroxides from groundwater flowing through the porous rock.
Uses & applications
Commonly used as a building material, for paving, in decorative masonry, and as a popular specimen for collectors due to its aesthetic banding.
Geological facts
Sandstone makes up about 20-25% of all sedimentary rocks on Earth. Banded sandstone is often marketed under names like 'Picture Sandstone' or 'Landscape Stone' when the patterns resemble natural scenery.
Field identification & locations
Identify in the field by its sand-like texture (feels gritty like sandpaper) and visible layering or rhythmic banding. Common in arid environments and ancient riverbeds.
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