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Bishop's Dyke is a linear earthwork located in Cumberland, England. The monument consists of a substantial bank and ditch that runs across the landscape, characteristic of early medieval defensive or territorial boundaries. Dating evidence and archaeological assessment suggest it belongs to the early medieval period, when such linear earthworks were constructed to demarcate land holdings or provide defensive barriers. The dyke represents an important example of the engineering and spatial organisation of early medieval northern England, though its precise original function and the identity of its constructors remain subjects of scholarly examination.
Bishop's Dyke is a scheduled monument protected by Historic England under reference 1007136. View the official record →
Bishop's Dyke is a linear earthwork located in Cumberland, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007136.
Bishop's Dyke 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 1007136.
Several scheduled monuments lie within 10 km, including Settlement 500yds (460m) SE of Cardew Hill (3.4 km), Rectangular enclosures 95yds (85m) N of Sceughmire (3.8 km), Oval enclosure 180m NE of Great Orton (4.5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Bishop's Dyke'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.
Bishop's Dyke stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is mudstone, siltstone and sandstone.