
sedimentary
Pale weathered pebble, likely limestone
Limestone, predominantly calcite (CaCO₃); exact identification is uncertain from the image
AI-generated identification · may be incorrectLight tan, dull to weakly earthy luster, fine-grained and rounded from abrasion; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity about 2.7. It may fizz with dilute hydrochloric acid or vinegar if fresh calcite is exposed.
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Physical properties
Light tan, dull to weakly earthy luster, fine-grained and rounded from abrasion; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity about 2.7. It may fizz with dilute hydrochloric acid or vinegar if fresh calcite is exposed.
Formation & geological history
Likely formed from compacted marine carbonate sediment and later rounded by stream, beach, or glacial transport; age cannot be determined visually and may range from recent to hundreds of millions of years.
Uses & applications
Commonly used for aggregate, cement, lime, building stone, and soil neutralization; this small ordinary pebble has little decorative or commercial value.
Geological facts
Limestone often contains microscopic fossils or shells, though none are visible here. Surface weathering can obscure its original texture and reduce the acid reaction.
Field identification & locations
Look for powdery pale surfaces, calcite grains or fossils, and effervescence in acid; distinguish it from quartzite, which is harder and will not fizz. Common worldwide, especially in former marine basins and river gravels.
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