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Cross dyke on Gerrick Moor is a linear earthwork monument situated on high moorland in Yorkshire. The dyke takes the form of a substantial bank and ditch, characteristic of defensive or boundary works constructed during the Iron Age or Romano-British period. Such moorland dykes served strategic functions as territorial markers, livestock enclosures, or defensive barriers protecting against incursion across exposed upland terrain. The monument remains a significant example of prehistoric or Romano-British land management and fortification practices in the northern Pennine region.
Cross dyke on Gerrick Moor, 690m north west of Black Beck Swang is a scheduled monument protected by Historic England under reference 1016992. View the official record →
Cross dyke on Gerrick Moor is a linear earthwork monument situated on high moorland in Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1016992.
Cross dyke on Gerrick Moor, 690m north west of Black Beck Swang 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 1016992.
Several scheduled monuments lie within 10 km, including Southern Pind Howe round barrow on Danby Rigg, 700m east of Rock House (7.2 km), High Stone Dike, southern of two cross dykes on Castleton Rigg (7.7 km), Wolf Pit round barrow at the southern end of Danby Rigg, 810m south east of Falcon Farm (7.8 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Cross dyke on Gerrick Moor, 690m north west of Black Beck Swang'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 Gerrick Moor, 690m north west of Black Beck Swang stands on Kellaways Formation And Oxford Clay Formation (Undifferentiated), bedrock that formed in the Oxfordian. The rock here is mudstone, siltstone and sandstone.