Sunday stone

Sunday Stone is the name given to layered deposits that formed inside drainage pipes from the coal mines of Durham and Northumberland. 

Sunday Stone: recording England's coal mining past

No bigger than a smartphone, this remarkable rock has layers that tell the story of the working lives and hardships of miners in the 1800s.

Tucked to one side of the Lasting Impressions gallery, this remarkable specimen is easily overlooked by visitors to the Museum.

It formed in a water trough at the bottom of a Tyneside coal mine in North East England.

As coal miners were busy labouring to supply Britain's rapidly expanding industry, their weekly routine was being recorded in stone.

William Smith's geological map 1815

A close up of an area of William Smith's 1815 geological map of England, Wales and Southern Scotland.
 

How did Sunday Stone form?

Sunday Stone is a calcareous deposit that formed as slowly flowing water deposited a white mineral (calcium carbonate) coating the drainage trough at the bottom of the mine.

When coal was extracted, the layers of carbonate laid down were blackened by the coal dust that filled the air in the mine during the working day. 

Coal specimen


 

What can it tell us about the working lives of miners?

The regular black-and-white striped pattern in Sunday Stone is a material record of the bleak working conditions experienced by coal miners in the nineteenth century.

Illustration of coal miners in England 1871

Illustration of coal miners in England 1871.

A pair of light and dark bands represents one 24-hour working day. The dark band marks each day shift in the heavy, dust-laden atmosphere, whereas the thinner, light band shows the hours of inactivity during the night.

Thicker, light-coloured bands appeared on Sundays, on holidays and at other interruptions in the mine when the water would run clean for 48 hours.

In these banded patterns you can see the ongoing struggle to improve mine safety and ventilation.

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Lasting impressions agate

See the Sunday Stone for yourself

It's currently on display in the Lasting Impressions gallery, outside of the British Geological Survey.