Crowbyres Bridge is a Grade C listed building in the Scottish Borders local planning authority area, Scotland. First listed on 7 November 2007.

Crowbyres Bridge

WRENN ID
seventh-clay-martin
Grade
C
Local Planning Authority
Scottish Borders
Constituency
Berwickshire, Roxburgh and Selkirk MP: John Lamont (Con)
Country
Scotland
Date first listed
7 November 2007
OS grid reference
NT 505 134
Coordinates
55.41236, -2.78326
Source
Historic Environment Scotland listing

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

Description

Crowbyres Bridge is a road bridge built in 1819 by John Smith of Darnick, with later widening in the 19th century. It consists of two segmental arches; the main span and a smaller flood arch to the north, crossing Slitrig Water. The bridge has splayed wing walls and triangular cutwaters. The structure is primarily random rubble stone, with some 20th-century rebuilding to the west side.

The bridge exemplifies John Smith's innovative economical method of whinstone rubble arch construction, which eschewed the use of ashlar. John Smith (1782-1864) and his brother Thomas were builders and architects working extensively in the Scottish Borders during the early 19th century, and their techniques were documented in the RIBA Transactions.

A ford previously existed at this location, as illustrated on Matthew Stobie’s map of Roxburghshire or Tiviotdale from 1770. Ainslie's map of 1821 shows the bridge in its original form. The bridge was widened to the west during the later 19th century, likely around 1870, as evidenced by neatly dressed voussoirs on the western elevation and Ordnance Survey maps. The clear distinction between the original construction and the later widening contributes to the architectural interest of the bridge. The bridge is located on a sharp corner of the B6399 between Hawick and Newcastleton, just south of Hawick. John Smith’s diary entry from 18th January 1819 refers to the bridge.

Local climate

Crowbyres Bridge sits in a wetter-than-average part of the UK, with an average of 1,010 mm of rain a year. This makes it wetter than 81% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 67% of listed buildings.

It experiences an average of 56 freeze-thaw cycles a year, more than 96% of listed buildings. Of these, 35 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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