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Hall Yards is a moated site located approximately 150 metres north-west of Tyrell's Hall in Cambridgeshire. The monument comprises a substantial rectangular moat that formerly enclosed a domestic or manorial establishment, typical of medieval settlement patterns in the region. Dating to the medieval period, the site represents a form of land tenure and residential arrangement common amongst gentry and substantial landholding families during the twelfth to sixteenth centuries. The moat itself survives as an earthwork feature, indicating the former presence of a house platform within its bounds, though the superstructure has not survived to modern times.
Moated site known as Hall Yards, 150m north west of Tyrell's Hall is a scheduled monument protected by Historic England under reference 1019549. View the official record →
Hall Yards is a moated site located approximately 150 metres north-west of Tyrell's Hall in Cambridgeshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1019549.
Moated site known as Hall Yards, 150m north west of Tyrell's Hall 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 1019549.
Several scheduled monuments lie within 10 km, including Springfield style enclosure, three bowl barrows and two pond barrows on Whiteley Hill (8.8 km), Earl's Hill bowl barrow: part of the round barrow cemetery on Therfield Heath (9 km), Two bowl barrows: part of the round barrow cemetery on Therfield Heath (9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Moated site known as Hall Yards, 150m north west of Tyrell's Hall'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.
Moated site known as Hall Yards, 150m north west of Tyrell's Hall stands on Grey Chalk Subgroup, bedrock that formed in the Cenomanian. The rock here is chalk.