Oxenfoord Bridge is a Grade B listed building in the Midlothian local planning authority area, Scotland. First listed on 18 October 1976.

Oxenfoord Bridge

WRENN ID
stubborn-pier-autumn
Grade
B
Local Planning Authority
Midlothian
Constituency
Midlothian MP: Kirsty McNeill (Lab)
Country
Scotland
Date first listed
18 October 1976
OS grid reference
NT 398 673
Coordinates
55.89552, -2.96319
Source
Historic Environment Scotland listing

Also on this page: flood risk · radon risk · weather exposure · detailed attributes ↓

Description

Oxenfoord Bridge is a single-span bridge dating to around 1800. Constructed with harled random rubble, it features ashlar copes and pink sandstone ashlar voussoirs for the segmental arch. The north and south principal elevations show sloped offsets with plain abutments supporting the segmental arch, featuring projecting imposts and an architvolt to the extrados. Partially harled rubble wing walls are present, topped with flattened stone copes, though some replacements are of grey concrete. The east and west elevations consist of sloped wing walls leading to a tarmac roadway uphill, which then flattens onto the bridge.

The bridge is now out of use and sits adjacent to a modern structure carrying traffic on the A6093, the main route to Pencaitland and Haddington. The boundary between the parishes of Cranston, Midlothian and Ormiston, East Lothian lies beyond the bridge. The bridge presents a plain design compared to other bridges in the area and was built before a major road construction phase in the parish. It's located near the site of what was the home farm of the old Oxenfoord Castle, though it was not part of an estate. References to the bridge appear on the Ordnance Survey First Edition map of 1856 and in Rev J Dickson’s “Cranstoun: A Parish History” (1907) on page 145.

Local climate

Oxenfoord Bridge receives an average of 960 mm of rain a year. This makes it wetter than 74% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 55% of listed buildings.

It experiences an average of 36 freeze-thaw cycles a year, more than 62% of listed buildings. Of these, 21 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.3°C per decade since 1991.

Averages for 1991–2020; temperature trend 1991–2025. Figures describe the wider area (a grid cell of roughly 10 km), not the individual site. Contains modified Copernicus Climate Change Service information 2026.

More on this building

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