
sedimentary
Sandstone (lithic wake/graywacke variety)
Arenite/Greywacke (SiO2 with lithic fragments)
AI-generated identification · may be incorrectHardness: 6-7 (Mohs); Color: Gray to brownish-gray; Luster: Dull/Earthy; Crystal Structure: Clastic (granular); Cleavage: None (fractures irregularly); Specific Gravity: 2.2-2.8
- Hardness
- 6-7 (Mohs)
- Color
- Gray to brownish-gray
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (Mohs); Color: Gray to brownish-gray; Luster: Dull/Earthy; Crystal Structure: Clastic (granular); Cleavage: None (fractures irregularly); Specific Gravity: 2.2-2.8
Formation & geological history
Formed through the accumulation and lithification of sand-sized mineral particles or rock fragments. This specimen appears to be a graywacke, typically formed in deep-water marine environments via turbidity currents.
Uses & applications
Commonly used as construction aggregate, road base, and occasionally as dimension stone for landscaping or building veneers.
Geological facts
Sandstone makes up about 20% of all sedimentary rocks on Earth. Graywacke varieties are often called 'dirty sandstone' because of the high concentration of clay and diverse rock fragments mixed with quartz.
Field identification & locations
Identify by its gritty texture (feels like sandpaper) and visible grains. It is commonly found in sedimentary basins and mountain belts. Collectors look for unique banding or fossil inclusions.
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