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Cunzierton Fort is an Iron Age hillfort situated in Roxburghshire, in the Borders region of Scotland. The fort occupies a naturally defensible position on bedrock composed of Silurian to Devonian extrusive rocks, specifically mafic lava and tuff formed during the Devonian period. This volcanic geology provides a substantial natural foundation for the monument, with the darker, harder stone characteristic of such deposits offering excellent defensive advantages.
The fort is protected as a scheduled monument under Historic Environment Scotland's national record, registered under reference SM2170. This designation recognises its archaeological significance as a surviving example of Iron Age fortified settlement in southeastern Scotland, a region rich in such defended sites dating broadly to the period between 800 BC and the Roman conquest of southern Britain.
Like other hillforts of its era, Cunzierton would have functioned as a settlement, refuge and administrative centre for the surrounding community. The specific topography and geology of this Roxburghshire location shaped how the Iron Age inhabitants adapted their defensive structures to the landscape, making it a distinctive local variant within the broader tradition of Iron Age fortification in northern Britain.
Cunzierton,fort is a scheduled monument protected by Historic Environment Scotland under reference SM2170. View the official record →
Cunzierton Fort is an Iron Age hillfort situated in Roxburghshire, in the Borders region of Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM2170.
Cunzierton,fort dates from the iron age period, and is classified as a fort. It is one of over 32,000 scheduled monuments protected across the UK.
Cunzierton,fort 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 SM2170.
Several scheduled monuments lie within 10 km, including Heugh Law, fort (5.7 km), Loddan Hill North, palisaded settlement 800m NNE of summit (5.8 km), Plenderleith, scooped settlement 300m SSW of (6 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Cunzierton,fort'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.
Cunzierton,fort stands on Unnamed Extrusive Rocks, Silurian To Devonian, bedrock that formed in the Devonian. The rock here is mafic lava and mafic tuff.