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Two moated sites and associated features 520m north of Grimston Garth is a medieval monument consisting of two separate moated enclosures located in North Yorkshire. The sites represent typical examples of medieval manorial or domestic settlement, with the moated platforms serving defensive and status-indicating functions characteristic of the 12th to 16th centuries. The associated features visible as earthworks include the water-filled or silted moats defining the enclosures, together with banks and ditches that formed integral parts of the medieval landscape organisation. Such paired moated sites in this region reflect the pattern of medieval landholding and settlement dispersal across the Yorkshire countryside.
Two moated sites and associated features 520m north of Grimston Garth is a scheduled monument protected by Historic England under reference 1021241. View the official record →
Two moated sites and associated features 520m north of Grimston Garth is a medieval monument consisting of two separate moated enclosures located in North Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1021241.
Two moated sites and associated features 520m north of Grimston Garth is a Scheduled Ancient Monument, legally protected by Historic England (NHLE) — the body responsible for designating and safeguarding heritage sites in England. The official designation reference is 1021241.
Several scheduled monuments lie within 10 km, including Shaw Fosse moated site (5.6 km), Roos Castle moated site and associated fishponds (6.1 km), Bewick Hall moated site (6.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Two moated sites and associated features 520m north of Grimston Garth'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.
Two moated sites and associated features 520m north of Grimston Garth stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.