
sedimentary
Weathered sandstone fragment
Quartz-rich sandstone, likely feldspathic or lithic sandstone
AI-generated identification · may be incorrectLight tan-gray, rough and granular with visible sand-sized grains and brown weathering; likely Mohs hardness ~6–7 overall, dull to slightly earthy luster, and no obvious cleavage. Individual quartz grains are hard, while the cement may be weaker.
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Physical properties
Light tan-gray, rough and granular with visible sand-sized grains and brown weathering; likely Mohs hardness ~6–7 overall, dull to slightly earthy luster, and no obvious cleavage. Individual quartz grains are hard, while the cement may be weaker.
Formation & geological history
Formed when sand accumulated, compacted, and cemented by silica, iron oxides, or carbonate, commonly in rivers, dunes, beaches, or shallow marine settings. Its exact geological age cannot be determined from the photograph.
Uses & applications
Used as building stone, paving, aggregate, and occasionally as a decorative stone; this small weathered fragment has negligible commercial or jewelry value.
Geological facts
Sandstone commonly preserves cross-bedding, ripple marks, fossils, and ancient environmental clues. Brown or reddish tones often reflect iron-oxide cement or weathering.
Field identification & locations
Identify it by its gritty texture and visible clastic grains; a steel nail may scratch weakly cemented sandstone, while quartz grains resist scratching. Common worldwide, especially in sedimentary basins and exposed cliffs.
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