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| 0437 |
The Pulse of Asia : vol.1 |
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OCR Text
grapher might say. The condition of the lake in his day was
probably very much the same as it is to-day. Later, how-
ever, there appears to have been a change. Near the south
shore of the lake there is a little island, on which stand the
ruins of an ancient Armenian monastery. Around it the
stone houses of an ancient village can be seen submerged in
water to a depth of twenty or thirty feet. Local tradition,
recorded in a book preserved till the massacres of 1895 in
a neighboring Armenian village, relates that the monastery
was built about A. D. 500 or 600, at which time the island
was part of the mainland. The present bed of the lake, so
the record goes, was a cultivated plain, through the middle
of which flowed a stream. The stream disappeared at the
lower end of the plain, but reappeared beyond the moun-
tains, where it joined the Euphrates. Gradually the under-
ground exit was closed with silt, and the plain was converted
into a lake. The reduced size of the lake at some historic
period is proved not only by the Armenian monastery, but
by a line of forts. The forts, which are from one to two
thousand years old, plainly mark the course of an impor-
tant road from Harput to Diarbekir running directly across
what is now the bed of the lake at a point about four miles
from its western end.
As to the supposed underground outlet, I could find no
proof of its existence, though I searched diligently. Never-
theless, in spite of the improbability that a lake which had
existed for ages, as is shown by its deposits in deltas and
beaches, should be drained by a temporary underground
outlet, which soon became clogged again, I accepted such
an hypothesis in 1900 as the most probable explanation.
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