
sedimentary
Limestone (River Pebble)
Calcium Carbonate (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: Light gray to tan; Luster: Dull/Earthy; Structure: Fine-grained/Microcrystalline; Specific Gravity: 2.5-2.7. It reacts via effervescence (fizzing) with dilute hydrochloric acid.
- Hardness
- 3 on Mohs scale
- Color
- Light gray to tan
- Luster
- Dull/Earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Light gray to tan; Luster: Dull/Earthy; Structure: Fine-grained/Microcrystalline; Specific Gravity: 2.5-2.7. It reacts via effervescence (fizzing) with dilute hydrochloric acid.
Formation & geological history
Formed through the accumulation of shell, coral, algal, and fecal debris in warm, shallow marine waters. This specific specimen is a river pebble, shaped by fluvial erosion which smoothed its edges over long periods of transport in water.
Uses & applications
Raw limestone is used in cement manufacturing, as a soil conditioner in agriculture, and as crushed stone for road bases. In its polished form, it is used for floor tiles and architectural facades.
Geological facts
Limestone makes up about 10% of the total volume of all sedimentary rocks. Most caves around the world are formed in limestone when acidic groundwater dissolves the rock over thousands of years.
Field identification & locations
Identify in the field by its soft surface (can be scratched by a steel nail) and its tendency to 'fizz' when a drop of vinegar or acid is applied. Commonly found in riverbeds, coastal areas, and ancient sea beds.
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