
sedimentary
Beige limestone tile
Limestone, primarily calcite (CaCO₃); exact variety cannot be determined from the image
AI-generated identification · may be incorrectPale beige-gray, matte, fine-grained surface with irregular veining and fossil-like markings; calcite hardness 3 Mohs, trigonal crystal structure, and typically good cleavage. The tile is cut and finished, so its surface appearance may not reflect the raw stone.
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Physical properties
Pale beige-gray, matte, fine-grained surface with irregular veining and fossil-like markings; calcite hardness 3 Mohs, trigonal crystal structure, and typically good cleavage. The tile is cut and finished, so its surface appearance may not reflect the raw stone.
Formation & geological history
Limestone forms from accumulated marine carbonate sediments and shells, later compacted and cemented; its age and source cannot be established visually. The rectangular, uniform piece is a human-cut building product.
Uses & applications
Commonly used for flooring, wall cladding, and architectural finishes; polished or distinctive limestone may also be used decoratively.
Geological facts
Limestone is composed chiefly of calcite and reacts with dilute acid by fizzing, though surface treatments can affect testing.
Field identification & locations
Look for carbonate fizz, relatively low hardness, and possible fossils or bedding; limestone is quarried worldwide. This appears to be an installed or sample tile, not a natural hand specimen.
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