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.
Herodotus speaks of the Malian plain (vii. 198) as being divided
into two parts by the projection of the mountain at either side. The
greatest and highest mass of Œta, west of the Trachinian cliffs,
extends northwards towards Othrys, and marks off the upper plain of
Hypati, the ancient Hypata, from the lower plain of Lamia. The breadth
of the plain where it is broadest, [which he states to be at the city
of Trachis,] he gives at a figure which has been corrupted in the text.
The actual breadth from the exit of the Asopos defile to Lamia is about
eight miles, or about four hundred plethra.
His account of the natural features of the district begins outside the
limits of the region which formed the scene of operations. The rivers
Dyras and Melas may be identified with sufficient certainty under the
modern names of Gourgo-potamo and Mavra-neria.
Herodotus now enters upon the description of those features which did
have an influence upon the events of 480 B.C. “South of Trachis,” he
says (vii. 199), “there is a cleft in the mountain range which shuts
in the territory of Trachinia; and the river Asopos, issuing from the
cleft, flows for a while along the foot of the hills.”
The Asopos, at the present day, after issuing from the ravine, turns
eastwards through an angle of at least 45 degrees, and proceeds for a
distance of about two and a half miles in the direction of the north
foot of the hills which form the west gate of Thermopylæ. There is a
sort of bay in the range between the ravine and the west gate of the
pass. Herodotus’ description of it as flowing along the foot of the
hills would be applicable to its course at the present day. Its bed, a
broad stony channel, thickly sown with bushes of oleander and plane,
is one which is liable to alteration; but I could not find any trace
or evidence whatever of its having largely diverged from its present
course within recent times; and the modern maps of this district which
represent the river as running far out into the plain before turning
towards Thermopylæ are certainly wrong. No really reliable map of the
region as a whole at present exists. The best I have seen is one in
Hauvette’s Herodotus; and that contains several palpable errors.
#ROUTE OF HERODOTUS.#
Public-domain text, read in full here on John Shaqi.
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