
Dry Burn enclosure - Satellite - LiDAR Finder
Dryburn Henge/Enclosure
Location and Landscape Context
Dryburn Henge lies on Alston Moor in Cumbria, within the North Pennines Area of Outstanding Natural Beauty. It occupies a strategic point on the high moor, being located at the very centre of Alston Moor, at a key strategic and routeway point. It is located roughly at NY 760 430, where routes across the Pennine watershed converge. The surrounding terrain is underlain by Carboniferous Great Scar Limestone and interbedded Yoredale Shales, with scattered fluvioglacial gravels in valley bottoms. Heather-clad moorland and peat bogs dominate the immediate vicinity, offering expansive views toward the Eden and Tyne valleys .
![]() Dry Burn enclosure - 1m Lidar - National Museum of Scotland |
![]() Dry Burn enclosure - OS Series 1 - National Museum of Scotland |
Geology and Geography
The henge’s builders chose a natural plateau on the limestone–shale interface, where shallow soils overlie weathered bedrock. Springs at this lithological junction provided water, while nearby copper-bearing veins in the limestone likely attracted Neolithic travellers. The moor’s upland environment suggests primarily seasonal use, with the henge serving as a focal point in a largely transhumant landscape .
Monument Structure
Dryburn Henge is a roughly circular Earthwork, measuring c. 40–45 m in diameter internally. Its defining features are:Inner bank: Made of turf-faced earth and cobble, standing up to 1 m high.
Internal ditch: Stands 4–5 m wide and 0.5–1 m deep, set just inside the bank.
Single entrance gap: Located on the southeast side, aligned with a likely trackway across the moor.
Subdued external counterscarp bank: Seen in places, marking what is assumed to be the original outer boundary .
No internal stone or timber settings have survived, and there is no visible central platform—suggesting Dryburn was a purely earthen henge (Class I type).
Dating and Archaeological Investigations
Altogether Archaeology (ASDU) undertook small-scale excavation and post-excavation analysis in 2016. Charcoal from the primary ditch fill produced radiocarbon dates in the late third millennium cal BC, placing Dryburn firmly in the terminal Neolithic (Chalcolithic) period . No associated occupation debris or structural remains were found, leaving its exact function open to interpretation.
Interpretation and Significance
Dryburn Henge’s location at a convergence of cross-Pennine routes implies it functioned as a ritual waypoint or meeting place for communities moving between the Eden and Tyne corridors. Its construction in a remote upland setting underscores the Neolithic emphasis on landscape marking far from settled lowlands. Because it provides one of the few radiocarbon-anchored examples of a small, earthen henge in the North Pennines, Dryburn expands our understanding of how ritual monuments punctuated travel and exchange networks across Britain’s high moors .
Reference
Paul Frodsham, Altogether Archaeology Fieldwork Module 1a. Dry Burn Enclosure. Project Design. Website version.















