A green headland and dark sea cliffs curving away above a rocky shore by Siccar Point under a pale blue sky.
Scottish Borders

Siccar Point

The rocky headland on the Berwickshire coast where James Hutton saw the proof of deep time in 1788, one of the most famous places in geology.

Welcome

Siccar Point looks like any other rocky headland on the Berwickshire coast, but it is one of the most important places in the history of science.

In 1788 the geologist James Hutton came here by boat and found the evidence that changed how we understand the age of the Earth.

On the point, dark grey rocks stand on end, formed on the floor of an ancient ocean. On top of them lie almost flat layers of red sandstone, laid down on land some 65 million years later. Between them is a line marking an old land surface where the lower rocks had been folded, lifted and worn away. Hutton saw that this must have taken unimaginable time. His friend John Playfair wrote that the mind grew giddy looking so far into the abyss of time.

The Edinburgh Geological Society opened its Deep Time Trail in 2026 to help visitors find the place and understand it. The final descent to the rocks is steep, so take care.

A short drive awayColdingham Beach CaféA small white café on the sand at Coldingham Bay near St Abbs, for coffee, milkshakes and cake beside the beach huts.17 min by roadSee itInside the beach café: wooden floor and tables, with chalkboard menus above the white counter.
Before you go

Open at any hour; the final descent to the rocks is steep.

Where
The Berwickshire coast near Cockburnspath.
Hutton
1788.
The gap
About 65 million years.
Stay nearby

Places to stay near the point, and when each is next free.

Hidden Scotland, the magazine

Scotland, in print.

Every photograph commissioned, every word written by somebody who went. Printed twice a year, made in Scotland.

Find out more

For further reading, before you go.