A type of Iron Age hillfort where the external walls of stone have become smooth by the heat of the sun or by burning, combined with windy conditions. The walls fuse into a slaggy or glassy mass, becoming vitrified. Dry-stone timber-laced ramparts, especially in Scotland, have timber-lacing that has been fired causing the stone core of the rampart to fuse. They are dated roughly in the last few centuries BC and early centuries AD.