
sedimentary
Sandstone (Quartzite-rich)
Clastic Sedimentary Rock (primarily SiO2)
Hardness: 6-7 on Mohs scale; Color: Tan, brown, and ochre with visible iron-oxide staining; Luster: Dull to earthy; Crystal structure: Granular/clastic texture; Cleavage: None; Specific gravity: Approx 2.65.
- Hardness
- 6-7 on Mohs scale
- Color
- Tan, brown, and ochre with visible iron-oxide staining
- Luster
- Dull to earthy
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Physical properties
Hardness: 6-7 on Mohs scale; Color: Tan, brown, and ochre with visible iron-oxide staining; Luster: Dull to earthy; Crystal structure: Granular/clastic texture; Cleavage: None; Specific gravity: Approx 2.65.
Formation & geological history
Formed through the accumulation and cementation of mineral particles (lithification) of sand-sized grains. This specimen shows significant rounding, suggesting a fluvial (river) or coastal origin where water energy smoothed the edges over time.
Uses & applications
Used in construction as a building material, in the glass-making industry (if pure quartz), and as decorative landscaping stones or garden features.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. The red/orange tints in this specific rock are caused by the oxidation of iron minerals, essentially acting as a natural rust that cements the sand grains together.
Field identification & locations
Identify in the field by its 'sandpaper' feel and visible grains. It is commonly found in riverbeds, canyons, and desert environments mapping ancient coastlines. Look for bedding planes or layers which are often visible in larger outcrops.
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