Ireland, Historic and PicturesqueJohnston, Charles
History
Ireland, Historic and Picturesque
Johnston, Charles
Ireland -- Description and travel; Ireland -- History
Such is the distribution of this once dominant but now dwindled race,
which has gradually descended from the summit of power as ancient Rome
descended, as Greece descended, or Assyria or Egypt. But we can look
back with certainty to a time when this race, and this race only, held
complete possession of all the lands we have mentioned, in north or
south, in Europe or northern Africa; holding everywhere to the Atlantic
coast, or, as in the Mediterranean isles, evidently pressing inward from
the Atlantic, past the Pillars of Hercules, through the Strait of
Gibraltar.
It is evident at once that the territory of this race corresponds
exactly, throughout many countries, with the territory of the cromlechs
and standing stones; where we find the one, as in Ireland, Brittany,
Spain, we find the other; where the one is absent, as in Germany, or
northern Italy or Greece, the other is likewise absent. The identity is
complete. We are justified, therefore, in giving the same provisional
name to both, and calling them Atlantean, from their evident origin not
far from Atlas, and their everywhere clinging to the Atlantic coast. We
can find traces of no other race which at all closely fulfills the
necessary conditions of uniform and undisputed extension, through a long
epoch, over the whole cromlech region--the only conditions under which
we can conceive of the erection of these gigantic monuments, or of the
long established and universally extended spiritual conditions which
make possible such vast ideal enterprises.
In this race, therefore, which we have called Atlantean, we find the
conditions fulfilled; of this race, and of no other, we still find a
lingering remnant in each of the cromlech countries; and we hardly find
a trace of this race, either now or in the past, in the lands which have
no cromlechs or standing stones.
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. We have given one mode
of reckoning already; we find it corroborated by another. In the Somme
valley, in northern France, we have a Nature's timepiece; in the peat,
at different levels, are relics of the Roman age; of the Gaulish age
which preceded it; and, far deeper, of pre-historic races, like our
Atlanteans, who preceded the Gauls. The date of the Roman remains we
know accurately; and from this standard we find that the peat grows
regularly some three centimeters a century, or a foot in a
thousand years.
Public-domain text, read in full here on John Shaqi.
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