The church, stone tower house and earthworks offer different historical perspectives on Kilsallaghan. The area’s history encompasses a church site with traces of earlier predecessors, a transfer in 1197, buildings from the 18th and early 19th centuries, and archaeological features. If you are looking for a holiday rental, this combination offers a clear thematic focus: the history of churches, buildings and landscapes.
Saint David’s Church: Building History and Earlier Traces
Saint David’s Church in Kilsallaghan is an Anglican Church of Ireland church dating from the early 19th century. It was built on the site of an earlier church within an enclosed graveyard. On its west side, it has a two-stage, battlemented entrance tower; inside is a stained-glass window dating from around 1900. The church building thus brings together several historical layers: the earlier church site, the architecture of the entrance tower and a later window element.
The church’s history also includes the year 1197, when Saint David’s Church was transferred to St Thomas’ Abbey in Dublin. Outside the graveyard wall are traces of a low, broad earthwork. These are probably the remains of a church enclosure, suggesting that the site predates the Anglo-Norman period. The possible enclosure and the 1197 transfer thus represent different phases in the area’s history.
Distinguishing Between the Tower House and the Motte
Kilsallaghan Castle and Kilsallaghan Motte offer a clear comparison between a stone building and an earthwork. The castle on the R122 Road in Castlefarm, Kilsallaghan, is the ruin of a medieval stone tower house. The motte is also on the R122 Road in Castlefarm, Kilsallaghan: it is a low, flat-topped earthen mound, possibly an Anglo-Norman motte. The two forms are therefore clearly distinct: the castle centres on the stone tower house, while the motte is defined by its earthen mound and its cautiously worded historical classification. Those interested in historic building methods can see the difference between a stone tower-house ruin and an earthwork here.
Former Rectory and Ringfort
Kilsallaghan Glebe adds a former rectory dating from the mid-18th century to the area’s building history. The property includes outbuildings and gateway structures. Its former use as a rectory adds another historic function to the area’s buildings.
Dunmucky Ringfort represents a different type of archaeological site. It is about 40 metres in diameter and surrounded by a deep ditch. Its approximate size and the ditch give the ringfort a distinct character among the earthworks described here. Together with the low Kilsallaghan Motte and the broad earthwork outside the graveyard wall, it allows for comparisons between different forms and cautious historical classifications.
County Fingal in a Wider Context
County Fingal provides the wider regional setting and adds a coastal dimension to travel planning. Its coastline stretches for 88 kilometres from Sutton to Balbriggan. It includes three protected estuaries, salt marshes and 13 larger beaches. Velvet Strand in Portmarnock is a five-kilometre-long sandy beach. Balcarrick Beach is 3.4 kilometres long and has sand, dunes and rock pools; Skerries South Strand is a two-kilometre-long sandy beach with a promenade and coastal path. These coastal features belong to County Fingal and offer a separate regional perspective alongside Kilsallaghan’s local history.
The Howth Cliff Path Loop is also a county-wide route description: it starts at Howth DART station, follows the cliffs to “The Summit” and returns via a path running parallel to the outward route. This places different themes side by side for trip planning: historic buildings and earthworks in Kilsallaghan, as well as coastal landscapes and a cliff walk in the wider county.
Discover more destinations: Tyrrelstown, Swords, Castleknock, Cloghran, Lusk, Ballyboughal, Gormanston, Garristown
For the wider travel overview: County Fingal.
