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Frizles Linn is a settlement located 850 metres east-south-east of Newton in Dumfriesshire, Scotland. The site sits on bedrock of the Stewartry Group, a geological formation of Early Permian age comprising sandstone, breccia and conglomerate. This mixed geology would have provided both building stone and a naturally drained location suitable for habitation. The settlement's position within the rolling landscape of upper Dumfriesshire reflects the pattern of rural occupation characteristic of this region, though the specific date and nature of settlement remain to be fully established through archaeological investigation. The site is protected as a scheduled monument under Historic Environment Scotland reference SM6193, ensuring the preservation of any structural remains and archaeological deposits that may survive beneath the present ground surface.
Frizles Linn, settlement 850m ESE of Newton is a scheduled monument protected by Historic Environment Scotland under reference SM6193. View the official record →
Frizles Linn is a settlement located 850 metres east-south-east of Newton in Dumfriesshire, Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM6193.
Frizles Linn, settlement 850m ESE of Newton 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 SM6193.
Several scheduled monuments lie within 10 km, including Benoaks, stone row 150m N of (6.8 km), Garpol Water Moated Homestead, 500m SW of Rosseta (7.2 km), Auchen Castle (7.3 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Frizles Linn, settlement 850m ESE of Newton'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.
Frizles Linn, settlement 850m ESE of Newton stands on Stewartry Group, bedrock that formed in the Early Permian. The rock here is sandstone, breccia and conglomerate.