
sedimentary
Sandstone Beach Pebble
Clastic Sedimentary Rock (primarily Quartz with Iron Oxide coating)
Hardness: 6-7 (Mohs); Color: Tan, yellowish-brown to orange (iron-stained); Luster: Dull/Earthy; Crystal Structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Tan, yellowish-brown to orange (iron-stained)
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Tan, yellowish-brown to orange (iron-stained); Luster: Dull/Earthy; Crystal Structure: Granular/Clastic; Cleavage: None; Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. This specimen shows significant rounding and smoothing from high-energy water transport (beach or river action). Geological age varies by region but is likely Paleozoic to Cenozoic.
Uses & applications
Common industrial uses for sandstone include construction aggregate, glass manufacturing (if high silica), and as a building stone. Smooth pebbles like this are often used in landscaping, home decor, or as 'worry stones'.
Geological facts
Sandstone acts as a natural filter for groundwater and is one of the most common types of sedimentary rock on Earth. The orange/yellow hue is specifically caused by the oxidation of iron-bearing minerals, commonly referred to as 'limonite stain'.
Field identification & locations
Identify by its gritty, sand-like texture when scratched and visible layers or banding. Often found on coastlines, riverbeds, and desert regions. Collectors often look for unique shapes or 'omars' (stones with circular pits).
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