Burghead is a peaceful coastal village on the shores of the Moray Firth in the north east of Scotland. Visit the Burghead Visitor Centre for a walk through local history from around 400 AD to the present day, explore the Pictish Burghead Fort, and see the Dark Age Burghead Well.
The Burning of the Clavie, a fire festival unique to Burghead, welcomes the New Year on 11 January each year. Burghead Bay is rich in wildlife, with whales, dolphins, porpoises and seals regularly seen in the waters off the headland.
Interpretation panels line the Moray Coastal Path between Burghead and Hopeman. St Aethan's Well, a historic spring on the headland, was carefully restored and remains part of the local heritage trail.
What to Explore
Burghead Headland Trust SCIO runs the visitor centre from a former coastguard lookout built within the ramparts of the ancient fort. Displays cover Pictish carvings, fishing heritage, the herring industry and the natural history of the Moray Firth.
Walk out to the Pictish fort site to see what remains of one of the largest strongholds in early medieval Scotland. The carved Burghead Well is a rare surviving monument from that period. Each January, the Burning of the Clavie draws visitors from across Scotland and beyond.
See our Moray Coastal Path walking guide for route notes, heritage stops and practical tips. The path links Burghead with Hopeman and Lossiemouth, passing sandstone cliffs, sea caves and viewpoints where dolphins and seals are often spotted. Interpretation along the route explains the geology, history and wildlife of the headland.
Geology & Geography of Burghead
The rocky coast from Burghead to Lossiemouth is formed from golden-coloured Permian and Triassic sandstone, unique in this part of Scotland. The coastline has been quarried for centuries because these sandstones make excellent building stone. Cliffs and sea caves line the shore, and some caves show evidence of use from Pictish times onwards. The rocks at Burghead are Triassic, about 240 million years old. These Burghead sand beds were deposited by an ancient river system. Look closely and you can see where channels eroded into the layers below, and pebbles carried by the river from nearby mountains.
Walking east along the Moray Coastal Path from Burghead towards Hopeman, you reach a red rock at the edge of the sea called Red Craig. This marks a fault between the Burghead beds and the older Hopeman beds.
The Hopeman beds are also sandstones, laid down by the wind as ancient dunes. Many tracks of ancient reptiles, older than the dinosaurs, have been found in the Hopeman beds.
Sea Level Changes
Since the end of the last ice age, sea levels have changed markedly around Burghead. At low tide on Burghead beach, exposed peat beds reveal tree trunks, roots and branches, showing that sea level was much lower when the trees grew here, probably around 7,000 years ago. Sea levels then rose to a point higher than today. When the Picts occupied Burghead, the high ground from Burghead to Lossiemouth would have formed an island.
Over time, sea levels fell as the land rose and Burghead became linked to the mainland again. For further reading, see the Laich of Moray Project.
