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Sand Hutton Cross is a boundary cross located approximately 600 metres north-east of the Old Vicarage in Sand Hutton, North Yorkshire. The monument dates to the medieval period and served a territorial function, marking parish or land boundaries as was common practice throughout northern England during the Middle Ages. The cross survives as a standing stone monument, though specific details of its current physical condition and original sculptural features remain documented in the heritage record maintained by Historic England under list entry number 1011748.
Sand Hutton Cross boundary cross 600m north east of the Old Vicarage is a scheduled monument protected by Historic England under reference 1011748. View the official record →
Sand Hutton Cross is a boundary cross located approximately 600 metres north-east of the Old Vicarage in Sand Hutton, North Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1011748.
Sand Hutton Cross boundary cross 600m north east of the Old Vicarage 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 1011748.
Several scheduled monuments lie within 10 km, including Topcliffe Bridge (6 km), Maiden Bower and Cock Lodge: a motte and bailey castle, moated site, windmill mound and associated linear outwork (6.8 km), Medieval moated site, fishponds and associated field system 125m south of Eldmire Cottage (7.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Sand Hutton Cross boundary cross 600m north east of the Old Vicarage'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.
Sand Hutton Cross boundary cross 600m north east of the Old Vicarage stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.