The great Persian War and its preliminaries : $b A study of the evidence, literary and topographicalGrundy, G. B. (George Beardoe)
History
The great Persian War and its preliminaries : $b A study of the evidence, literary and topographical
Grundy, G. B. (George Beardoe)
Greece -- History -- Persian Wars, 500-449 B.C.
Immediately east of the Asopos defile the chain of Œta is at its
lowest, barely three thousand feet high, and it is over this part of
the range that the modern road is carried. The difficulties of passing
it do not, however, decrease in proportion to its height, and no
military way or path seems to have been practicable at this point.[109]
Farther east the range rises again into peaks of nearly five thousand
feet, faced towards the north by the great cliffs which overhang the
pass of Thermopylæ. #MT. ŒTA AND THE ASOPOS RAVINE.# Here the Malian
Gulf and not the plain forms the foreground of the picture, across
which, at a distance of eight or nine miles, a white line can be
discerned at the base of the cliffs, the great sulphur deposit of the
warm springs. This part of the Œta range was known as Kallidromos.
Away beyond Thermopylæ it extends towards the Euripus under the name
of Knemis, gradually bending in a more southerly direction down the
channel, until it is lost in the distance towards Atalanta. Behind it
and above it rises the great grey mass of Parnassus.
This very difficult range is rather turned than pierced by the pass of
Thermopylæ, the actual passage through the chain being many miles south
of the pass itself.
There is one point with reference to it which is not always recognized.
There was and is a second pass[110] through it leading direct to the
Dorian plain by way of the great ravine of the Asopos, a pass, too, of
which the Persian army actually made use after Thermopylæ had been won.
It would seem strange at first sight that the Persian generals, when
they found Thermopylæ so hard to force, did not nullify the defence of
it by marching into Doris this way.
The defile of the Asopos issues abruptly on to the Malian plain some
three and a half to four miles west of the Western Gate of Thermopylæ.
Its bottom is merely formed of the stony river bed, at first some fifty
yards wide, but rapidly contracting, until a little farther up the
chasm it is only twelve feet wide between absolutely sheer cliffs from
seven to nine hundred feet high. This winding rift in the mountains
continues for some three and a half miles from the entrance, and then
suddenly broadens out into a wide upland valley, behind the range of
Œta, from which there is a long but not difficult passage to the Dorian
plain.[111] This valley was, no doubt, the land of those Œteans whom
Thucydides mentions in his account of the circumstances leading to the
foundation of Heraklea Trachinia.
Public-domain text, read in full here on John Shaqi.
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