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At Cavancarragh, on the shoulder of Toppid Mountain, some four miles from Enniskillen, there is one of these circles; a ring of huge stone boulders with equal spaces between stone and stone. A four-fold avenue of great blocks stretches away from it along the shoulder of the hill, ending quite abruptly at the edge of a ravine, the steep channel of a torrent.
On the mountain side, as at Cavancarragh, the growth is likely to be slower than in a river valley; yet we may take the same rate, a foot a thousand years, and we shall have, for this great stone circle, an antiquity of ten or twelve thousand years at least.
We have already seen that the standing stones of Cavancarragh, four miles from Fermanagh, were, within the memory of men still living or of their fathers, buried under ten or twelve feet of peat, which had evidently formed there after their erection. We have here a natural chronometer; for we know the rate at which peat forms, and we can, therefore, assign a certain age to a given depth.
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