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St Albans Abbey Gatehouse is a fourteenth-century structure forming part of the monastic precinct of St Albans Abbey in Hertfordshire. Built in the 1360s, the gatehouse served as the principal entrance to the abbey's outer court and exemplifies the architectural conventions of high medieval monastery design. The structure is constructed in flint and stone with considerable decorative detailing characteristic of the period, featuring a central archway of substantial proportions suited to controlling access to the precinct. As one of the few surviving components of the abbey's original monastic architecture following the Dissolution of the Monasteries, the gatehouse remains significant testimony to the scale and sophistication of this major Benedictine foundation, which had been among England's most important religious houses since its Anglo-Saxon origins.
St Albans Abbey Gatehouse is a scheduled monument protected by Historic England under reference 1003523. View the official record →
St Albans Abbey Gatehouse is a fourteenth-century structure forming part of the monastic precinct of St Albans Abbey in Hertfordshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1003523.
St Albans Abbey Gatehouse 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 1003523.
Several scheduled monuments lie within 10 km, including The Clock Tower (0.3 km), St Albans Abbey, site of conventual buildings (0.3 km), Verulamium, part of wall and ditch of Roman city (0.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of St Albans Abbey Gatehouse'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.
St Albans Abbey Gatehouse stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.