
sedimentary
Sandstone (with Lichen)
Arenite (primarily SiO2)
AI-generated identification · may be incorrectHardness: 6-7 (individual quartz grains); Color: Tan, beige, brown, and weathered grey; Luster: Dull/Earthy; Crystal Structure: Clastic (composed of cemented grains); Cleavage: None; Specific Gravity: 2.2 - 2.8.
- Hardness
- 6-7 (individual quartz grains)
- Color
- Tan, beige, brown, and weathered grey
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (individual quartz grains); Color: Tan, beige, brown, and weathered grey; Luster: Dull/Earthy; Crystal Structure: Clastic (composed of cemented grains); Cleavage: None; Specific Gravity: 2.2 - 2.8.
Formation & geological history
Formed through the accumulation, compaction, and cementation of sand-sized mineral grains or rock fragments (weathering products). Common in desert, river, and marine environments over millions of years.
Uses & applications
Extensively used as a building stone, paving material, and in the production of glass (if high purity quartz). Also a major reservoir for groundwater and petroleum.
Geological facts
Sandstone reveals much about earth history, reflecting past environments such as ancient dunes or riverbeds. The white and yellow spotting on the surface is not a mineral part of the rock, but crustose lichen, a symbiotic organism of algae and fungi.
Field identification & locations
Identify in the field by its gritty 'sandpaper' feel and visible layers (bedding). It is found worldwide in sedimentary basins. Collectors often look for colorful 'wonderstone' varieties or those containing fossils.
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Sedimentary Sandstone
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