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Remains of East Haimes House and the adjacent section of the deer park pale is a post-medieval domestic and landscape monument located in Dorset. The site comprises the structural remains of a house and an associated section of pale fencing that formed part of a deer park enclosure, reflecting the status and recreational practices of its proprietors during the post-medieval period. The deer park pale, a substantial boundary constructed to contain deer stocks, demonstrates the significance of managed hunting grounds to the local landholding class. The monument preserves evidence of both domestic habitation and the landscape management practices characteristic of early modern rural estates.
Remains of East Haimes House and the adjacent section of the deer park pale is a scheduled monument protected by Historic England under reference 1465898. View the official record →
Remains of East Haimes House and the adjacent section of the deer park pale is a post-medieval domestic and landscape monument located in Dorset. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1465898.
Remains of East Haimes House and the adjacent section of the deer park pale 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 1465898.
Several scheduled monuments lie within 10 km, including King's Court Palace moated site (0.7 km), Gillingham Park boundary bank (2.5 km), Longbury long barrow 600m north west of Slaughtergate Farm (3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Remains of East Haimes House and the adjacent section of the deer park pale'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 East Haimes House and the adjacent section of the deer park pale stands on West Walton Formation, Ampthill Clay Formation And Kimmeridge Clay Formation (Undifferentiated), bedrock that formed in the Kimmeridgian. The rock here is mudstone, siltstone and sandstone.