
sedimentary
Sandstone (Quartzose Sandstone)
Arenite (primarily SiO2 with minor Fe2O3)
AI-generated identification · may be incorrectHardness: 6-7 (Mohs scale), Color: Tan to light brown with visible layering, Luster: Dull/Earthy, Crystal Structure: Granular/Clastic texture, Mineralogy: Mostly quartz grains with some feldspar and iron oxide cement.
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Physical properties
Hardness: 6-7 (Mohs scale), Color: Tan to light brown with visible layering, Luster: Dull/Earthy, Crystal Structure: Granular/Clastic texture, Mineralogy: Mostly quartz grains with some feldspar and iron oxide cement.
Formation & geological history
Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. Clastic particles are deposited by water, wind, or ice and then lithified under pressure. This specimen shows significant rounding, suggesting a fluvial (river) or beach origin where it was tumbled by water.
Uses & applications
Commonly used as a building material, paving stone, and in the production of glass (if high quartz purity). It also serves as a significant reservoir rock for groundwater and petroleum.
Geological facts
Sandstone makes up about 10-20% of the Earth's sedimentary rocks. Its color is often determined by the cementing material; the brownish hue in this specimen suggests a presence of iron oxide (hematite or limonite).
Field identification & locations
Identify in the field by its 'sandpaper' feel and visible bedding planes (layering). It can be found globally in riverbeds, deserts, and coastal regions. For collectors, look for cross-bedding or fossil inclusions.
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