Killyvally Bridge, Bridge Street, Garvagh, Coleraine, Co Londonderry, BT51 is a Grade B2 listed building in the Causeway Coast and Glens local planning authority area, Northern Ireland. First listed on 25 September 1978.

Killyvally Bridge, Bridge Street, Garvagh, Coleraine, Co Londonderry, BT51

WRENN ID
gilded-quoin-coral
Grade
B2
Local Planning Authority
Causeway Coast and Glens
Constituency
East Londonderry MP: Mr Gregory Campbell (DUP)
Country
Northern Ireland
Date first listed
25 September 1978
Irish grid reference
C 842 158
Coordinates
54.98328, -6.68544
Source
NI Environment Agency listing

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Description

Killyvally Bridge is a four-arch masonry road bridge spanning the Agivey River at the east end of Garvagh, built in two distinct phases that reflect contrasting construction methods and periods.

The original bridge was constructed in the early 19th century on the downstream (north) side. This section is built throughout in random rubble basalt, with stones that are generally rounded, suggesting they were collected from the earth rather than quarried. The piers feature angled cutwaters that rise to arch spring level and taper towards the top. The four segmental arches are fitted with split stone voussoirs. The two central arches are slightly wider and higher than those at the ends. The parapet has dressed stone copings with a small drain hole at the centre, and a metal plaque bearing the bridge's name is fixed to the east end. Plastic planters line the top of the parapet.

Later in the 19th century, the bridge was widened by extending it upstream. The upstream section shows a markedly different architectural treatment, with squared basalt rubble forming the abutments, piers and arch soffits, while the spandrels and parapets are of undressed rubble. This squared stonework, more sharply angular than the downstream side, indicates stone from a quarry. The piers on this face have curved cutwaters capped with sandstone, rising to arch spring level. The arches match the downstream arches in size and profile but have rock-faced voussoirs and squared rubble soffits. The parapet carries dressed sandstone copings, a metal name plate at the west end, and planters. A small metal commemorative plaque commemorating someone possibly drowned nearby is attached to the upstream spandrel above the middle pier. A clear break in construction is visible along the abutments, piers and arch soffits between the two phases.

The slightly curved deck accommodates two traffic lanes and a footpath along each parapet. An unsurfaced ramp bounded by a random rubble basalt wall provides access to the upstream left bank. A low weir stands just downstream, built to prevent the river bed from eroding downward in the bridge vicinity.

Historical records show a road crossing the river at this location on Taylor & Skinner's 1777 map. The 1832 Ordnance Survey map clearly depicts a bridge, and the 1836 Ordnance Survey Memoir notes that an 18th-century bridge was swept away by flood around 1802 and subsequently rebuilt. The memoir describes it as 15 feet across with five arches, one of which served as a tailrace for a corn mill just upstream on the right bank. The name Killyvally Bridge is explicitly noted from the 1848-53 Ordnance Survey map onwards. By comparing the 1905 map with the 1853 edition, the upstream widening can be dated to the intervening period, bringing the bridge to its present width of approximately 30 feet.

The bridge forms part of the main road into Garvagh from the east and is situated at a location of local historical significance. A graveyard stands at the upstream west end. On the downstream side at this end are a car park, public toilets and a drain outfall. Gardens occupy both sides of the east end.

Local climate

Killyvally Bridge, Bridge Street, Garvagh, Coleraine, Co Londonderry, BT51 sits in a wetter-than-average part of the UK, with an average of 1,140 mm of rain a year. This makes it wetter than 89% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 75% of listed buildings.

It experiences an average of 15 freeze-thaw cycles a year, fewer than 85% of listed buildings. Of these, 10 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.2°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.

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