Rock Identifier
Weathered sandstone or quartz-rich sedimentary rock (Indeterminate sandstone; commonly quartz–feldspar framework grains cemented by silica, calcite, or iron oxides) — sedimentary
sedimentary

Weathered sandstone or quartz-rich sedimentary rock

Indeterminate sandstone; commonly quartz–feldspar framework grains cemented by silica, calcite, or iron oxides

AI-generated identification · may be incorrect

Tan-gray, dull to faintly gritty surface with possible fine bedding or weathering bands; likely hardness 6–7 for quartz-rich grains, variable porosity, and no obvious cleavage. The rounded shape appears naturally weathered or transported.

Identified More sedimentary
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Physical properties

Tan-gray, dull to faintly gritty surface with possible fine bedding or weathering bands; likely hardness 6–7 for quartz-rich grains, variable porosity, and no obvious cleavage. The rounded shape appears naturally weathered or transported.

Formation & geological history

Formed from compacted and cemented sand-sized sediment, probably deposited in a river, shoreline, dune, or floodplain environment; age cannot be determined from the photograph.

Uses & applications

Common sandstone is used as building stone, paving, aggregate, and occasionally sculpture material; this piece has little commercial value without unusual texture, fossils, or provenance.

Geological facts

The image does not show diagnostic fossils or clear sedimentary structures, so exact identification requires a fresh surface, grain inspection, and acid testing for carbonate cement.

Field identification & locations

Look for visible sand grains, layered bedding, and a gritty fracture; quartz-rich sandstone scratches glass, while carbonate-cemented varieties may fizz with dilute hydrochloric acid. Sandstone occurs worldwide, especially in sedimentary basins.