It sits at the eastern edge of a terrace, orientated roughly north-north-east to south-south-west, and from that position it looks out over the Irish Sea. The view may or may not have mattered to whoever raised it. The tilt almost certainly did not; that is simply what several thousand years of settling ground will do to a stone.

The monument itself is composed of Greywacke, a coarse-grained metamorphic conglomerate common to the local geology of Wicklow. What makes this particular stone visually distinctive is its surface: a pale white ground overlaid with orange staining, the result of long exposure and weathering. Where the base has been slightly chipped, the original grey colour of the stone shows through, offering a glimpse of what it would have looked like when first set upright. It measures 1.9 metres in length and stands 1.7 metres high, with a maximum thickness of around half a metre, making it a moderately substantial example of its type. Standing stones of this kind are scattered across the Irish landscape and are broadly prehistoric in date, though pinning down their original purpose is rarely straightforward; they have been associated with territorial markers, burial sites, astronomical alignments, and routeways, often without firm evidence for any one explanation at a given site.