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Blackpark cross dyke and standing stone is a prehistoric monument located near Blackpark Lodge in Yorkshire. The site comprises a cross dyke, a linear earthwork characteristic of Iron Age defensive works, alongside a standing stone of probable prehistoric date. Such cross dykes are typically interpreted as territorial boundaries or defensive barriers constructed during the Iron Age period, though precise dating and function remain subjects of archaeological study. The monument represents evidence of early settlement patterns and landscape organisation in this region of Yorkshire during the prehistoric period.
Blackpark cross dyke and standing stone, 330m north east of Blackpark Lodge is a scheduled monument protected by Historic England under reference 1018594. View the official record →
Blackpark cross dyke and standing stone is a prehistoric monument located near Blackpark Lodge in Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1018594.
Blackpark cross dyke and standing stone, 330m north east of Blackpark Lodge 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 1018594.
Several scheduled monuments lie within 10 km, including High Cross wayside cross on Kirkgate Lane, north of Appleton-le-Moors (3.1 km), Nutholm cross dyke, 100m south of Appleton Mill Farm (3.4 km), Low Cross, a reused standing stone on Kirkgate Lane in Appleton-le-Moors (3.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Blackpark cross dyke and standing stone, 330m north east of Blackpark Lodge'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.
Blackpark cross dyke and standing stone, 330m north east of Blackpark Lodge stands on Ravenscar Group, bedrock that formed in the Bathonian. The rock here is sandstone, siltstone and mudstone.