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Packhorse Bridge at the Post Office is a small stone bridge located in Westmorland, dating to the medieval period. The structure is characteristic of packhorse bridges that served as vital transport routes across difficult terrain in the Pennine region, enabling the movement of goods by pack animal before the establishment of modern road networks. Built from local stone with a typically narrow, arched design suited to foot and animal traffic rather than wheeled vehicles, the bridge reflects the commercial and agricultural importance of upland routes during the medieval and early modern periods. Such bridges remain significant archaeological witnesses to the organisation of medieval trade and communication networks in northern England.
Packhorse bridge at the Post Office is a scheduled monument protected by Historic England under reference 1007138. View the official record →
Packhorse Bridge at the Post Office is a small stone bridge located in Westmorland, dating to the medieval period. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007138.
Packhorse bridge at the Post Office 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 1007138.
Several scheduled monuments lie within 10 km, including Hincaster Tunnel horse path (1.5 km), Basingill gunpowder works, 130m south of Force Bridge (1.8 km), Levens Park, round barrows and medieval settlements, including Temple of Diana (1.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Packhorse bridge at the Post Office'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.
Packhorse bridge at the Post Office stands on Dinantian Rocks (Undifferentiated), bedrock that formed in the Mississippian. The rock here is limestone with subordinate sandstone and argillaceous rocks.