Ringfort (Rath), Meelick, Co. Mayo
Co. Mayo |
Ringforts
A ringfort that actively resists inspection has a certain logic to it.
The rath at Meelick sits on a knoll in undulating pasture in County Mayo, positioned so that its north-eastern and eastern sides drop away sharply into natural slope, lending the site a defensive quality that its builders may well have intended. What strikes you, even before you get close, is that this is not a place that has settled quietly into the landscape. It commands open views northward over Killala Bay, and its earthworks remain substantial enough to read clearly in the ground.
A rath is an early medieval enclosure, typically of the first millennium AD, formed by one or more earthen banks and ditches and used as a farmstead or high-status residence. At Meelick, the circular interior measures roughly 36 to 40 metres across and is defined by an inner bank, a fosse (the ditch immediately outside it), and an outer bank beyond that. The inner bank reaches around 5.6 metres wide on the north-western side, and the whole system of banks and ditch is well preserved, though the eastern and south-eastern sections are complicated by the natural fall of the ground, where the man-made earthworks and the steep slope begin to merge. A gap of about two metres in the inner bank at the south-south-east, matched by a corresponding gap in the outer bank, appears to mark the original entrance. Inside, slightly south-east of centre, there is a souterrain, a type of stone-lined underground passage or chamber commonly associated with raths and thought to have served for storage or concealment. It is visible now as a stone-lined depression. Two further sites lie close by: another enclosure around 150 metres to the west-north-west, and a possible rath on a rise about 200 metres to the west-south-west, suggesting this knoll was part of a broader pattern of early settlement in the area.
The interior is currently choked with blackthorn, hawthorn, and brambles, and the perimeter is equally dense, making the earthworks difficult to examine in any detail on the ground. The souterrain, the entrance gaps, and the relationship between the outer bank and the natural slope to the north-east are the features most worth trying to trace, though the vegetation makes all of this a matter of patient looking rather than easy reading.
