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Tughall is a deserted medieval village and chapel site located in Northumberland, England. The settlement dates from the medieval period and represents evidence of human habitation and religious practice that was subsequently abandoned, leaving behind archaeological remains that contribute to understanding rural settlement patterns in northern England. The site comprises earthwork features indicative of a former village layout alongside the remains of a chapel, which together testify to the organized community structure that once existed at this location. Such deserted medieval villages are significant for revealing the processes of settlement abandonment and landscape change during and after the medieval period.
Deserted medieval village and chapel at Tughall is a scheduled monument protected by Historic England under reference 1014732. View the official record →
Tughall is a deserted medieval village and chapel site located in Northumberland, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1014732.
Deserted medieval village and chapel at Tughall 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 1014732.
Several scheduled monuments lie within 10 km, including Dovecote S of Glebe Farm (4.6 km), North Charlton medieval village and open field system (5.6 km), Prehistoric burial mound, 420m north west of East Linkhall (6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Deserted medieval village and chapel at Tughall'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.
Deserted medieval village and chapel at Tughall stands on Yoredale Group, bedrock that formed in the Bashkirian. The rock here is limestone with subordinate sandstone and argillaceous rocks.