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Askham Fell stone alignment is a Neolithic or Bronze Age monument located in Westmorland, comprising a linear arrangement of standing stones on the fell landscape. The alignment consists of several stones set in a deliberate pattern, reflecting prehistoric ritual or territorial practices common to upland areas of northern England during these periods. Such alignments are interpreted by archaeologists as having served ceremonial, astronomical, or boundary-marking functions within Neolithic and Bronze Age communities. The monument remains significant as evidence of early settlement and land use in the Lake District region and contributes to understanding prehistoric stone arrangements in the north of England.
Askham Fell stone alignment is a scheduled monument protected by Historic England under reference 1007376. View the official record →
Askham Fell stone alignment is a Neolithic or Bronze Age monument located in Westmorland, comprising a linear arrangement of standing stones on the fell landscape. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007376.
Askham Fell stone alignment 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 1007376.
Several scheduled monuments lie within 10 km, including Enclosure containing four clearance cairns and a stone bank west of Four Stones Hill (6.1 km), Round cairn west of enclosure on Four Stones Hill (6.1 km), Round cairn on Burn Banks (6.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Askham Fell stone alignment'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.
Askham Fell stone alignment stands on Dinantian Rocks (Undifferentiated), bedrock that formed in the Mississippian. The rock here is sandstone, limestone and argillaceous rocks.