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Souterrains 100m SW of Ardownie Farm Cottages is an Iron Age underground stone-built structure located in Angus, Scotland. The monument comprises a subterranean passage or chamber typical of souterrain construction, a building form characteristic of northern Britain during the Iron Age, particularly the first few centuries AD. Such structures served various functions including storage, refuge, or ritual purposes, and their presence reflects the settlement patterns and architectural practices of Iron Age communities in eastern Scotland. The site represents an important example of prehistoric underground architecture in the region and contributes to understanding of Iron Age settlement and material culture in Angus.
Souterrains 100m SW of Ardownie Farm Cottages is a scheduled monument protected by Historic Environment Scotland under reference SM6512. View the official record →
Souterrains 100m SW of Ardownie Farm Cottages is an Iron Age underground stone-built structure located in Angus, Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM6512.
Souterrains 100m SW of Ardownie Farm Cottages 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 SM6512.
Several scheduled monuments lie within 10 km, including Fetterdale, unenclosed settlement 300m NW of (8.3 km), Morton, timber hall and enclosure 240m SSE of (8.5 km), Morton, Mesolithic settlement 350m SE of (8.5 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Souterrains 100m SW of Ardownie Farm Cottages'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.
Souterrains 100m SW of Ardownie Farm Cottages stands on Unnamed Extrusive Rocks, Silurian To Devonian, bedrock that formed in the Devonian. The rock here is mafic lava and mafic tuff.