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Slight univallate hillfort 150m east of Cleeve Court is a modest Iron Age defensive enclosure located in Somerset, England. The site is defined by a single bank and ditch forming its fortification, characteristic of univallate hillforts common across the region during the Iron Age period. The slight preservation of its earthworks suggests either original modest construction or considerable degradation over the intervening centuries. Its location near Cleeve Court positions it within the broader landscape of Iron Age settlement and territorial control in Somerset.
Slight univallate hillfort 150m east of Cleeve Court is a scheduled monument protected by Historic England under reference 1011263. View the official record →
Slight univallate hillfort 150m east of Cleeve Court is a modest Iron Age defensive enclosure located in Somerset, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1011263.
Slight univallate hillfort 150m east of Cleeve Court 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 1011263.
Several scheduled monuments lie within 10 km, including Bowl barrow 190m south west of Tyning's Farm: part of the Tyning's Farm round barrow cemetery (9.3 km), Group of three bowl barrows 180m south of Tyning's Farm: part of the Tyning's Farm round barrow cemetery (9.4 km), Bowl barrow 250m south east of Tyning's Farm: part of the Tyning's Farm round barrow cemetery (9.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Slight univallate hillfort 150m east of Cleeve Court'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.
Slight univallate hillfort 150m east of Cleeve Court stands on Dinantian Rocks (Undifferentiated), bedrock that formed in the Mississippian. The rock here is limestone with subordinate sandstone and argillaceous rocks.