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Castle Hill is a univallate hillfort situated within Kirklees Park in Yorkshire, England. The monument consists of a single defensive bank and ditch enclosure crowning the summit of elevated ground, a defensive configuration characteristic of Iron Age settlement practice in northern Britain. The site demonstrates the strategic placement of such fortified settlements, occupying commanding topography typical of the period. The univallate design suggests a relatively modest defensive installation, possibly serving a community of limited size or representing a particular phase of occupation within a broader chronological sequence of settlement activity in the region.
Castle Hill univallate defended settlement, Kirklees Park is a scheduled monument protected by Historic England under reference 1005806. View the official record →
Castle Hill is a univallate hillfort situated within Kirklees Park in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1005806.
Castle Hill univallate defended settlement, Kirklees Park 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 1005806.
Several scheduled monuments lie within 10 km, including Kirklees Priory, medieval nunnery (0.4 km), Anglian high cross fragment known as Walton Cross (2.1 km), Anglian high cross fragment in the churchyard of St Matthew's Church, Rastrick (3.5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Castle Hill univallate defended settlement, Kirklees Park'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.
Castle Hill univallate defended settlement, Kirklees Park stands on Pennine Lower Coal Measures Formation And South Wales Lower Coal Measures Formation (Undifferentiated), bedrock that formed in the Westphalian. The rock here is mudstone, siltstone, sandstone, coal, ironstone and ferricrete.