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Wardlaw Hill is a prehistoric earthwork located south-south-west of Harpercroft in Ayrshire, Scotland. The monument is protected by Historic Environment Scotland as a scheduled monument under reference SM307. The site occupies elevated ground underlain by Carboniferous to Permian igneous bedrock, specifically a mafic intrusion that provides a hard, durable foundation typical of the upland terrain in this region of south-west Scotland.
The earthwork represents a substantial defensive or ceremonial structure from the prehistoric period, positioned to command views across the surrounding landscape. The choice of location on igneous bedrock would have offered natural advantages for construction, with the solid stone base providing stability for substantial ramparts or banks. Such elevated positions were strategically valuable for communities during the Bronze and Iron Ages.
The monument's survival as an identifiable earthwork attests to its original substantial construction. Protected status ensures that this important record of prehistoric settlement and land use in Ayrshire is preserved for future study and understanding of how early communities organised and defended their territories in south-west Scotland.
Wardlaw Hill,earthwork SSW of Harpercroft is a scheduled monument protected by Historic Environment Scotland under reference SM307. View the official record →
Wardlaw Hill is a prehistoric earthwork located south-south-west of Harpercroft in Ayrshire, Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM307.
Wardlaw Hill,earthwork SSW of Harpercroft 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 SM307.
Several scheduled monuments lie within 10 km, including Wardlaw Hill,earthwork W of Harpercroft (0.3 km), Kemp Law,fort (1.2 km), Dundonald Castle (2 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Wardlaw Hill,earthwork SSW of Harpercroft'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.
Wardlaw Hill,earthwork SSW of Harpercroft stands on Unnamed Igneous Intrusion, Carboniferous To Permian, bedrock that formed in the Permian. The rock here is mafic igneous-rock.