King Arthur's Seat
Arthur's Seat is the highest point in Edinburgh and one of the most prominent urban hills in Europe, an ancient volcano rising 251 metres above the city centre within Holyrood Park that provides panoramic views across Edinburgh, the Firth of Forth and the surrounding Lothian landscape from a summit accessible to walkers of all abilities within minutes of the city's major attractions. The hill takes its name from the legendary King Arthur, one of several locations across Britain that claim association with the mythological figure, and the combination of the dramatic volcanic topography, the panoramic views and the historical connections of the park make Arthur's Seat one of Edinburgh's most rewarding outdoor experiences.
The volcanic geology of Arthur's Seat is one of its most interesting features. The hill is the eroded remnant of a volcano that was active approximately 350 million years ago and whose lavas and intrusive igneous rocks were sculpted by glacial erosion during successive ice ages into the craggy profile visible today. The Salisbury Crags, the prominent line of dolerite cliffs below the main summit, were the subject of the geological observations made by James Hutton in the late eighteenth century that helped establish the science of geology and the concept of deep geological time, making this hill one of the birthplaces of modern earth science.
The summit of Arthur's Seat is reached by several routes, the most popular ascending from St Margaret's Loch through the Gutted Haddie gully to the summit ridge, a walk of approximately forty-five minutes from the Holyrood Palace car park. The panorama from the top on a clear day is extraordinary, encompassing the full extent of Edinburgh from the castle to the Firth of Forth, the Bass Rock offshore and the hills of Fife across the water.