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Mill of Kincraggie is a ring ditch located in Aberdeenshire, situated approximately 450 metres north-east of the mill itself. Ring ditches of this type are characteristic Bronze Age monuments, typically representing the levelled remains of barrows or the outer boundaries of prehistoric settlements. The earthwork survives as a circular or oval ditch, which would originally have enclosed a raised platform or been part of a ceremonial or domestic landscape.
The monument occupies ground underlain by a felsic igneous intrusion of Late Silurian to Early Devonian age, formed during the Early Devonian period. This bedrock geology, characteristic of Aberdeenshire's complex geological heritage, would have influenced prehistoric settlement patterns and land use in the area. The specific location and soil conditions created by this underlying geology are factors that would have shaped human activity at this site.
The ring ditch is protected by Historic Environment Scotland as a scheduled monument under reference SM8587, recognising its significance as evidence of prehistoric activity and land division in the region. Such monuments contribute to understanding Bronze Age settlement, ceremonial practices and agricultural organisation across north-east Scotland.
Mill of Kincraggie, ring ditch 450m NE of is a scheduled monument protected by Historic Environment Scotland under reference SM8587. View the official record →
Mill of Kincraggie is a ring ditch located in Aberdeenshire, situated approximately 450 metres north-east of the mill itself. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM8587.
Mill of Kincraggie, ring ditch 450m NE of 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 SM8587.
Several scheduled monuments lie within 10 km, including North Gellan,settlement and field system 350m N of (1.2 km), Coull Castle (1.9 km), Blue Cairn, long cairn 750m ESE of Tillyduke (3.6 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Mill of Kincraggie, ring ditch 450m NE of'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.
Mill of Kincraggie, ring ditch 450m NE of stands on Unnamed Igneous Intrusion, Late Silurian To Early Devonian, bedrock that formed in the Early Devonian. The rock here is felsic-rock.