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0423 Ruins of Desert Cathay : vol.2
中国砂漠地帯の遺跡 : vol.2
Ruins of Desert Cathay : vol.2 / 423 ページ(カラー画像)

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doi: 10.20676/00000213
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hold and the end of the Hao-shan-k'ou spur northward, were
manifestly built for this purpose. Judging from the shape
and arrangement of their sun-dried bricks, these advanced
towers did not look of a very remote age. Yet their state
of decay and the signs of successive repairs plainly indi-
cated that they were older than the wall extending behind
them. For the latter it seemed difficult to assume a greater
antiquity than that of Ming times, as local tradition asserts ;
so well preserved were the main wall itself and the enclos-
ures of the towers which served as quarters and rallying-
points for the men guarding it.
The disposition of the loopholes in the crenellated clay
parapet suggested defence by firearms. Otherwise these
towers built inside the wall and adjoining it showed but
little departure from the principles of fortification illustrated
by the ancient Limes in the desert. There was the same
solid cone of stamped clay, some thirty-four feet square at
the base, with a lightly built watch-room on the top. A
double line of foot-holes ascending one of the sides was
intended to help the watchmen who had to climb up by a
rope. Within the enclosure, some sixty feet square, which
guarded the tower, were small quarters for soldiers, now
ruined. The main wall showed at its foot a thickness of
eleven feet, and with its parapet rose to sixteen feet.
It was at the very first of these towers of the wall,
situated only some two miles beyond the great Gate, that
I struck the remains of the far more decayed wall, previously
referred to, running south-west to north-east. Closer in-
spection at once proved that my assumption of a different,
and probably far earlier, date of construction was correct.
This wall, which had only a thickness of eight or nine feet
on the ground and reached a height of ten or eleven
feet, was also built of stamped clay. But whereas the clay
layers in the wall closing the Chia-yü-kuan valley were four
or five inches in height, those in the older wall touching it
here at right angles were fully ten to twelve inches thick.
These measurements at once recalled the almost identical
ones observed in the rampart north and west of Tun-huang,
which my explorations of the spring had proved to be of
early Han times. The conclusion thus suggested received