
sedimentary
Likely sandstone
Quartz-rich sandstone, probably arkosic or lithic sandstone
AI-generated identification · may be incorrectFine- to medium-grained, dull tan-gray, and weakly consolidated; likely quartz with feldspar and rock fragments in a cementing matrix. Mohs hardness is roughly 6–7 for grains, with earthy luster and no obvious cleavage; exact texture is obscured by dim lighting.
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Physical properties
Fine- to medium-grained, dull tan-gray, and weakly consolidated; likely quartz with feldspar and rock fragments in a cementing matrix. Mohs hardness is roughly 6–7 for grains, with earthy luster and no obvious cleavage; exact texture is obscured by dim lighting.
Formation & geological history
Formed when sand accumulated, was compacted, and cemented in a river, dune, beach, or shallow-marine setting. Its age cannot be determined from the photograph and may range from Precambrian to recent geological formations.
Uses & applications
Used as building stone, paving, aggregate, and a source of silica; attractive varieties are used decoratively. This ordinary fragment has minimal commercial or collector value.
Geological facts
Sandstone commonly preserves ripple marks, cross-bedding, burrows, and fossils. Iron-oxide cement often produces red or brown coloration, while this specimen appears relatively weakly colored.
Field identification & locations
Look for visible sand grains, gritty texture, bedding, and a granular fracture; a streak or acid test can help distinguish it from limestone, while a hand lens improves identification. Common worldwide, especially in sedimentary basins.
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