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Cross dyke on Saltergate Brow is an ancient linear earthwork situated in Yorkshire. The monument consists of a substantial bank and ditch arrangement that runs across the landscape, characteristic of Iron Age defensive or boundary constructions. Such dykes typically functioned to control movement across terrain or to demarcate territorial divisions during the prehistoric period. The structure's preservation as a scheduled monument reflects its archaeological significance as evidence of Iron Age settlement patterns and land use in the region.
Cross dyke on Saltergate Brow, 750m south east of Barr Farm is a scheduled monument protected by Historic England under reference 1021166. View the official record →
Cross dyke on Saltergate Brow is an ancient linear earthwork situated in Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1021166.
Cross dyke on Saltergate Brow, 750m south east of Barr Farm 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 1021166.
Several scheduled monuments lie within 10 km, including Two prehistoric linear boundaries with associated features, 680m ESE and 880m NNE of Pexton Moor Farm (9.2 km), Warrening enclosure 975m north east of High Paper Mill Farm (9.2 km), Warrening enclosure 1.08km north east of High Paper Mill Farm (9.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Cross dyke on Saltergate Brow, 750m south east of Barr Farm'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.
Cross dyke on Saltergate Brow, 750m south east of Barr Farm stands on Corallian Group, bedrock that formed in the Oxfordian. The rock here is limestone, sandstone, siltstone and mudstone.