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Gidlow Hall moated site is a medieval moated enclosure located near Aspull in Lancashire. The site consists of a substantial rectangular moat which formerly surrounded a residential dwelling, representing a form of domestic fortification typical of the medieval period in northern England. Moated sites of this character were commonly constructed by minor gentry and prosperous landowners from the twelfth century onwards, serving both defensive and status-conferring functions. The Gidlow moat survives as an important archaeological record of medieval settlement patterns and social hierarchy in the Lancashire landscape.
Gidlow Hall moated site, Aspull, 560m NNE of Pennington Hall is a scheduled monument protected by Historic England under reference 1014210. View the official record →
Gidlow Hall moated site is a medieval moated enclosure located near Aspull in Lancashire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1014210.
Gidlow Hall moated site, Aspull, 560m NNE of Pennington 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 1014210.
Several scheduled monuments lie within 10 km, including The Moat House moated site 600m WNW of St David's Church (3.2 km), Haigh Sough mine drainage portal, 310m west of Park House (3.4 km), Mabs Cross on Standishgate, 20m west of Mabs Cross School building (4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Gidlow Hall moated site, Aspull, 560m NNE of Pennington 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.
Gidlow Hall moated site, Aspull, 560m NNE of Pennington Hall 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.