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Deil's Dike is a linear earthwork located on the Hill of Ochiltree in Wigtownshire, south-west Scotland. The monument consists of a substantial ditch and bank arrangement typical of early medieval or medieval field boundaries in the region. Its construction would have exploited the underlying Kirkcolm Formation wacke bedrock, a hard sandstone that outcrops across this area and provides stable foundations for such earthworks.
The monument sits within the distinctive landscape of south Wigtownshire, where similar linear features often mark ancient territorial divisions or property boundaries. The rolling terrain and exposed wacke geology would have made ditch excavation laborious, suggesting that Deil's Dike represents a significant investment in landscape management and suggests its importance as a boundary marker of considerable antiquity.
The site is afforded statutory protection as a scheduled monument under Historic Environment Scotland reference SM1966, recognising its value to understanding medieval or earlier land-use patterns in south-west Scotland. The monument remains a visible feature in the Ochiltree landscape, contributing to our understanding of how communities ordered and divided their territory in the medieval period.
Deil's Dike,linear earthwork,Hill of Ochiltree is a scheduled monument protected by Historic Environment Scotland under reference SM1966. View the official record →
Deil's Dike is a linear earthwork located on the Hill of Ochiltree in Wigtownshire, south-west Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM1966.
Deil's Dike,linear earthwork,Hill of Ochiltree is a Scheduled Ancient Monument, legally protected by Historic Environment Scotland — the body responsible for designating and safeguarding heritage sites in Scotland. The official designation reference is SM1966.
Several scheduled monuments lie within 10 km, including Loch Ochiltree,crannogs (1.2 km), Middle Bridge of Cree,cairn 110m WNW of (3.3 km), Loch Maberry Castle,crannog (4.4 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Deil's Dike,linear earthwork,Hill of Ochiltree's history, each drawn from the record and mapped to the exact spot:
Every location is different. Not every section appears for every place, only what the historical record actually holds turns up in a report.
Deil's Dike,linear earthwork,Hill of Ochiltree stands on Kirkcolm Formation, bedrock that formed in the Caradocian. The rock here is wacke.