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Offa's Dyke is a linear earthwork forming part of the extensive defensive frontier constructed during the reign of King Offa of Mercia in the late eighth century. This section, preserved within Wyeseal Wood north of Gumbers Land Barn, comprises a substantial bank and ditch that would have served to demarcate and defend the Anglo-Saxon kingdom's western boundary against Welsh territories. The monument exemplifies the characteristic engineering of the dyke system, which extends for approximately 149 kilometres along the England-Wales border. As a scheduled ancient monument, this stretch retains archaeological significance for understanding early medieval territorial control and the physical infrastructure of Offa's military and political ambitions.
Offa's Dyke: section in Wyeseal Wood, 600m north of Gumbers Land Barn is a scheduled monument protected by Historic England under reference 1020527. View the official record →
Offa's Dyke is a linear earthwork forming part of the extensive defensive frontier constructed during the reign of King Offa of Mercia in the late eighth century. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1020527.
Offa's Dyke: section in Wyeseal Wood, 600m north of Gumbers Land Barn 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 1020527.
Several scheduled monuments lie within 10 km, including Offa's Dyke: section in Danehill Wood, 300m west of East Vaga (7.8 km), Gaer Hill Camp, Penterry (8.3 km), Wyndcliff Roman Site (8.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Offa's Dyke: section in Wyeseal Wood, 600m north of Gumbers Land Barn'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.
Offa's Dyke: section in Wyeseal Wood, 600m north of Gumbers Land Barn stands on Lower Devonian Rocks (Undifferentiated), bedrock that formed in the Early Devonian. The rock here is sandstone and conglomerate, interbedded.