
South [Pic] is on the right side of the local hilltop, which is a very sensitive indicator for the winter solstice. North is across the valley, well to the right of the high point, at a bit of a break in the slope [Pic].
To the north-east, major standstillsLunistice positions vary cyclically over an 18.6 year period but are fairly static for more than a year at either end of the range
rise from a dip, minor ones from a step. The solstice is on a top, summer cross-quarters are at the left end of one.
The circle axis is well beyond the lunar limit in this direction [Pic].
Eastwards, the equinox is indicated by a hilltop and the month centred on it is well marked. Summer and winter cross-quarters are at the left end of hilltops.
The midpoints between them and the equinox are also usefully marked.
A tall, thin stone on this side and a matched pair on the other make an axial indicator for the summer cross-quarters [Pic].
Winter cross-quarters and minor standstillsLunistice positions vary cyclically over an 18.6 year period but are fairly static for more than a year at either end of the range
are both on the south-eastern hilltop though the highest point marks a quarter-month.
To either side, basal steps make high precision indicators for the cross-quarters and lunar major eighths.
A wide, flat-topped stone makes an axial indicator in this direction for the space between winter cross-quarters and minor standstillLunistice positions vary cyclically over an 18.6 year period but are fairly static for more than a year at either end of the range [Pic] but the reverse is beyond the north-west lunar limit [Pic].
To the south-west, winter solstice is on a hilltop. Minor standstillsLunistice positions vary cyclically over an 18.6 year period but are fairly static for more than a year at either end of the range
are in a dip and an intersect notch makes another high precision indicator for the major eighth, mirroring the south-east.
Due to the high horizon, southern lunisticesLunistices are the most northerly and southerly moons of the month. The lunar equivalent of solstices - more.
are not visible at all for about four and a half years at the major end of the cycle.
The circle axis indicates lunisticeLunistices are the most northerly and southerly moons of the month. The lunar equivalent of solstices - more. sets, particularly the major eighth [Pic]. The boulder axis is a bit more to the west but the difference is not obviously significant [Pic].
Westwards, the equinox, winter cross-quarters and equinox / cross-quarter midpoints all have reasonable markers but the quarter and half months get better ones.
A matched pair of stones on this side and a tall thin one on the other make an axial indicator for the equinox / winter cross-quarter midpoint [Pic].
North-western lunisticesLunistices are the most northerly and southerly moons of the month. The lunar equivalent of solstices - more.
fail to reach the hilltop. Minor standstillsLunistice positions vary cyclically over an 18.6 year period but are fairly static for more than a year at either end of the range
are indicated by a small notch. The step that begins the sequence is a half-month before Bealtaine, after Lughnasadh.
There are some more megalithic sites in the general area but the nearest surveyed ones are:
- Derrynafinchin Stone Circle is over the hills to the south, c.9km @ 150°
- Uragh Five Stone Circle is along Kenmare Bay to the west, c.19km @ 249°
- Gortanimill Stone Circle is over the hills to the east, c.21km @ 77°
References
- Archaeological Survey of Ireland, record details. www.archaeology.ie/archaeological-survey-ireland
- BYRNE, ELIZABETH et al. 2009 Archaeological Inventory of County Kerry, Volume I: South-West Kerry. Dublin: Stationary Office. p16, no.64.
- Ó'NUALLÁIN, SEÁN 1984 A Survey of Stone Circles in Cork and Kerry. Proceedings of the Royal Irish Academy 84c:1-77, p27, no.43.
- Ó'NUALLÁIN, SEÁN 1978 Boulder-Burials. Proceedings of the Royal Irish Academy 78c:75-114, p97, no.37.
- RUGGLES, C.L.N. 1999 Astronomy in Prehistoric Britain and Ireland. Newhaven & London: Yale University Press. No.ASC15.