Studies in Greek Scenery, Legend and History: Selected from His Commentary on Pausanias' 'Description of Greece,'Frazer, James George
History
Studies in Greek Scenery, Legend and History: Selected from His Commentary on Pausanias' 'Description of Greece,'
Frazer, James George
Greece -- Antiquities; Greece -- Description and travel
LXXXIII. TITHOREA.—The site of Tithorea, first identified by Clarke in
1801, is occupied by the modern village of Velitsa, which stands very
picturesquely among trees on the north-eastern slopes of Parnassus,
overlooking the broad valley of the Cephisus. About two-thirds of the
village are enclosed within the ancient ivy-mantled walls, which rank
with those of Messene and Eleutherae as among the finest existing
specimens of Greek fortifications. At the back of the village to the
south rises a huge mountainous cliff of grey rock, its ledges tufted
with pines. Between the foot of this great cliff and the village there
intervenes a very steep slope, mostly overgrown with holly-oak bushes.
On the east the village as well as the site of the ancient city is
bounded by a very deep rocky ravine, which winds southward into the
heart of the mountains. At the bottom of the ravine a torrent flows from
Parnassus over a broad gravelly bed to join the Cephisus in the plain
below. This torrent, now called Kakorevma or Evil Stream, is the ancient
Cachales. In the time of Pausanias, the townspeople, he tells us, had to
fetch their water in buckets from the depths of the lyn. Nowadays a
portion of the water of the stream is diverted higher up the glen and
brought in a conduit to the village, where it turns two mills and waters
the gardens and orchards. As Tithorea was thus naturally defended on two
sides, namely by the great cliff on the south and by the deep ravine on
the east, it needed walls on two sides only, the west and the north.
These walls, starting from the foot of the cliff, first descend the
steep slope in a straight line above the village, then follow the
gentler slope within the village, still in a direction due north, till
they turn round at an obtuse angle and run eastward to the brink of the
ravine. Here they stop. Along the edge of the ravine a number of ancient
blocks may be observed, but whether they are the remains of an ancient
fortification wall is not clear. Perhaps the deep precipitous side of
the ravine may have been considered a sufficient defence by itself. The
walls so far as they exist are finely and solidly built of regular
ashlar masonry, and are flanked by massive square towers constructed in
the same style. Walls and towers are best preserved in the lower ground
among the houses and gardens of the village, but on the steep slope
above the village the remains are also considerable.
Public-domain text, read in full here on John Shaqi.
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