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Building crop mark, possibly Corbier Hall, is a prehistoric or Romano-British archaeological site located in Kent, England. The monument is identified primarily through aerial photography and crop mark evidence rather than visible structural remains, a recognition method that has proven essential for understanding settlement patterns in the county. The site's precise dating and function remain uncertain given the nature of the archaeological evidence, though the crop marks suggest enclosures or structures of potential Iron Age, Romano-British, or early medieval date. Such cropmark sites represent important records of otherwise buried archaeological deposits and contribute significantly to understanding the landscape history and settlement distribution of the Kent region.
Building crop mark, possibly 'Corbier Hall' is a scheduled monument protected by Historic England under reference 1004188. View the official record →
Building crop mark, possibly Corbier Hall, is a prehistoric or Romano-British archaeological site located in Kent, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1004188.
Building crop mark, possibly 'Corbier 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 1004188.
Several scheduled monuments lie within 10 km, including Thurnham motte and bailey castle (1.3 km), Medieval moated site, Ripple Manor (1.8 km), Cistercian Abbey at Boxley (4.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Building crop mark, possibly 'Corbier 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.
Building crop mark, possibly 'Corbier Hall' stands on Gault Formation And Upper Greensand Formation (Undifferentiated), bedrock that formed in the Cenomanian. The rock here is mudstone, sandstone and limestone.