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Earthworks centring on 320 yards north-west of the Junction Inn, Efflinch is a scheduled ancient monument in Staffordshire comprising substantial ground features of archaeological significance. The site represents earthwork remains of undetermined period, though such features in this locality are typically associated with prehistoric or medieval activity. The monument's exact dating and functional interpretation require archaeological investigation, though its scheduling reflects recognition of its potential to contribute to understanding of landscape use and settlement patterns in the region. The earthworks remain visible as topographical features within the modern landscape near Efflinch.
Earthworks centring on 320yds (300m) NW of the Junction Inn, Efflinch is a scheduled monument protected by Historic England under reference 1006093. View the official record →
Earthworks centring on 320 yards north-west of the Junction Inn, Efflinch is a scheduled ancient monument in Staffordshire comprising substantial ground features of archaeological significance.
Earthworks centring on 320yds (300m) NW of the Junction Inn, Efflinch 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 1006093.
Several scheduled monuments lie within 10 km, including Enclosures and cursus 300yds (270m) SE of Efflinch (0.7 km), Pit alignments running NE and SW centring 320yds (300m) N of Wychnor Bridge (1 km), Timber circle, hengi-form monument and part of a pit alignment at Catholme (1.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Earthworks centring on 320yds (300m) NW of the Junction Inn, Efflinch'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.
Earthworks centring on 320yds (300m) NW of the Junction Inn, Efflinch stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is mudstone, siltstone and sandstone.