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The remains of All Saints Church, located 60 metres north-west of Stanway Hall Farm in Essex, is a scheduled ancient monument representing the site of a medieval parish church. The structure dates from the medieval period, though the exact phases of construction and any earlier Saxon origins remain subjects of archaeological enquiry. Physical remains at the site include fragmentary stonework and earthwork features indicative of a former ecclesiastical building, with the church long since fallen into disuse and decay. The monument's archaeological significance lies in its potential to illuminate patterns of medieval settlement and religious organisation within this part of Essex, though extensive excavation and detailed study would be required to establish its full chronological sequence and constructional history.
Remains of All Saints Church, 60m north-west of Stanway Hall Farm is a scheduled monument protected by Historic England under reference 1019879. View the official record →
The remains of All Saints Church, located 60 metres north-west of Stanway Hall Farm in Essex, is a scheduled ancient monument representing the site of a medieval parish church.
Remains of All Saints Church, 60m north-west of Stanway Hall Farm 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 1019879.
Several scheduled monuments lie within 10 km, including Gosbecks Iron Age and Romano-British site (1.3 km), Remains of St Mary's Church (1.3 km), Dovecote 80m south west of Olivers (1.5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Remains of All Saints Church, 60m north-west of Stanway Hall Farm'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.
Remains of All Saints Church, 60m north-west of Stanway Hall Farm stands on Thames Group, bedrock that formed in the Eocene. The rock here is clay, silt, sand and gravel.