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Attraction · Edinburgh, United Kingdom

Arthur's Seat

Arthur's Seat is a real extinct volcano rising 822 feet above Edinburgh within Holyrood Park, formed around 350 million years ago and later carved by glaciers into its current shape. A network of trails leads to the summit, with the most popular route taking most hikers roughly one to two hours round trip. On a clear day, the summit offers sweeping views across Edinburgh, the Firth of Forth, and out toward the surrounding countryside.

Photos of Arthur's Seat

Visitor guide

About Arthur's Seat

Arthur's Seat is an extinct volcano and the main peak of the hills that make up Holyrood Park in Edinburgh, Scotland, about a mile east of Edinburgh Castle. Rising to roughly 251 metres, it gives wide views over the city and the Firth of Forth and is one of Edinburgh's best-known hillwalks.

A Volcano in the City

Arthur's Seat is the largest part of the Arthur's Seat Volcano Site of Special Scientific Interest, which also includes Calton Hill and Castle Rock. Wikipedia dates the volcanic system to the early Carboniferous period, with lava samples dated to 341 to 335 million years ago. During the Quaternary, a glacier moving from west to east eroded the hill, exposing rocky crags on the west side, which became Salisbury Crags, and leaving a tail of material to the east. From some angles the hill resembles a lion lying down, with two extinct vents forming the Lion's Head and Lion's Haunch.

Hutton's Section, in Salisbury Crags, shows dolerite sills where magma pushed through sedimentary rock. Observations here by James Hutton helped shape modern geology.

The grassy volcanic peak of Arthur's Seat rising above Holyrood Park framed by tree branches

A Name and a Legend

An early name recorded in the charters of Holyrood Abbey is Craggenmarf. The name Arthur's Seat is sometimes said to come from legends about King Arthur, but this is presented as a claim rather than a confirmed origin, and similar names appear elsewhere in Britain. The earliest known Arthurian-style form, Arthurissete, appears in a 1508 work by Walter Kennedy. The hill is often cited as one possible location for Camelot, which is a tradition rather than a historical finding.

A high view over Arthur's Seat's crags with Edinburgh Castle and the city visible in the distance

Human History

A hill fort occupies the summit area, with further defences visible at Dunsapie Hill and above Samson's Ribs; these are of prehistoric date. They may have been centres of power for the Votadini, the people of the poem Y Gododdin. Cultivation terraces can be seen from Duddingston. On 1 May 1590 a bonfire on Salisbury Crags celebrated the safe return of James VI and Anne of Denmark.

The Radical Road runs beneath Salisbury Crags and was built after the Radical War of 1820 using unemployed weavers, following a suggestion by Walter Scott. In 1836 five boys found 17 miniature coffins containing small wooden figures in a cave on the crags; their purpose remains unknown, and the surviving coffins are in the National Museum of Scotland.

Tradition says David I, while hunting nearby, saw a vision of a cross between a stag's antlers and founded Holyrood Abbey. Young Edinburgh women also traditionally washed their faces in May Day dew on the slopes, a custom celebrated in Robert Fergusson's 1773 poem Caller Water.

Visiting the Hill

The easiest ascent is from the east, up a grassy slope above Dunsapie Loch. Historic Environment Scotland looks after the surrounding park. Robert Louis Stevenson described the hill as one for magnitude, a mountain in virtue of its bold design. Conditions can be windy and the paths uneven, so sturdy footwear is sensible; a private guide with a driver can drop you at a convenient starting point.

Frequently Asked Questions About Arthur's Seat

Arthur's Seat is about 251 metres (823 feet) high according to Wikipedia, with a prominence of 174 metres.
Yes, Arthur's Seat is an extinct volcano from the early Carboniferous period. Lava samples have been dated to roughly 335 to 341 million years ago.
It is sometimes said the name comes from King Arthur legends, but this is a claim rather than a proven origin. An earlier recorded name was Craggenmarf.
Salisbury Crags are dolerite cliffs, the exposed edge of an igneous sill, between Arthur's Seat and Edinburgh city centre, formed when a glacier eroded the hill. Hutton's Section there helped shape modern geology.
Holyrood Park is the royal park in Edinburgh that includes Arthur's Seat and Salisbury Crags, looked after by Historic Environment Scotland.
Wikipedia describes the easiest ascent as from the east, up the grassy slope above Dunsapie Loch.
The Radical Road is a path beneath Salisbury Crags, built after the Radical War of 1820 using unemployed weavers on a suggestion by Walter Scott.
In 1836 boys found 17 tiny coffins with wooden figures in a cave on Salisbury Crags. Their purpose is unknown and the surviving ones are in the National Museum of Scotland.
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