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Why does limestone get layer?

Updated: 8/11/2023
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11y ago

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The layers are known as "beds".

Limestone is one of the Sedimentary class of rocks, which start as sediments on, usually, the floor of a sea or lake.

Most limestones, including chalk, are from sea-bed accumulations of silt rich in Calcium Carbonate. Over time their own dead weight compresses them, driving out the water and initiating a process of "Lithification" - chemical and physical changes that turn the soft sediment into hard rock.

That's the rock made. Now to emplace it...

Summarising, over geological time, Earth-movements uplift the former sea-beds into hills and mountains, where the weather promptly starts to weather and erode them back into sediment for transport by rivers or glaciers back to the sea to start the cycle anew...

The beds simply reflect the original sediment deposits: changes in sediment supplies or characteristics, often reflecting climate changes, break the steady deposition to form interruptions known as "bedding planes".

The beds are all generally horizontal to start with, but the uplift processes is often accompanied by folding and faulting that can tilt the beds up at angles, in some cases even past 90 degrees so they slope "upside down".

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9y ago

Limestone is principally constructed of marine animals, so depending upon the location of the deposit, so it may be the oldest layer in that location. Limestone is sedimentary.

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