Harper's New Monthly Magazine, Vol. V, No. XXIX., October, 1852 — John Shaqi
Harper's New Monthly Magazine, Vol. V, No. XXIX., October, 1852Various
Religion
Harper's New Monthly Magazine, Vol. V, No. XXIX., October, 1852
Various
American literature -- Periodicals; Civilization -- Periodicals; Culture -- Periodicals
After remaining for some time at the encampment, Robinson and his
companions set out at five o'clock, to go down to the shore. The
declivity was still steep, though less so than in the pass above. The
ground was fertile, and bore many plants and trees, and the surface
of it appeared to have been once terraced for tillage and gardens. At
one place, near the foot of the descent, were the ruins of an ancient
town. From the base of the declivity, there was a rich and fertile
plain which lay sloping gradually nearly half a mile to the shore. The
bed of the brook could be traced across this plain to the sea, though
at the season of this visit, the waters which the fountain supplied,
copious as they appeared where they first issued from the rock, were
absorbed by the earth long before they reached the shore. The rivulet,
therefore, of Ain Jidy is the most short-lived and transitory of
streams. It breaks forth suddenly from the earth at its fountain, and
then, after tumbling and foaming for a short distance over its rocky
bed, it descends again into the ground, disappearing as suddenly and
mysteriously as it came into being.
The plain which this evanescent stream thus gave up its life to
fertilize, was all under cultivation at the time that Robinson visited
it, being divided into gardens, which belonged to a certain tribe of
wandering Arabs. This tribe were, however, not now encamped here, but
had gone away to a tract of ground belonging to them in another part
of the country, having left only a few sentinels to watch the fruits
that were growing in the gardens. Robinson and his party went across
the plain, and finally came to the margin of the sea, approaching it at
last over a bank of pebbles which lined the shore, and formed a sort of
ridge of sand and shingle, six or eight feet higher than the level of
the water. The slope of these pebbles, on the seaward side, was covered
with saline incrustations.
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