Haifa; or, Life in modern PalestineOliphant, Laurence
History
Haifa; or, Life in modern Palestine
Oliphant, Laurence
Palestine -- Description and travel
In regard to the engineering difficulties, so far as they are known, the
only records of levels which we have of the elevation of the land
between the Red Sea and the Dead Sea are those made at different times
by three Frenchmen—Mons. Lartet, Mons. Vigne, and Mons. Luynes. These
only differ nineteen feet—the lowest being seven hundred and eighty-one
feet, the highest eight hundred; but it must be remembered that these
are not the result of actual survey, but of rough estimates, and there
may be depressions in the dividing ridge which may have escaped these
gentlemen's observation.^[2] The dividing ridge is said to be calcareous
rock—the summit level distant fifty-two miles from the Red Sea and
fifty-eight from the Dead Sea, which is nearly thirteen hundred feet
lower than the level of the ocean—and it is assumed that the engineering
work would be facilitated by the scour which would be caused by the sea
rushing down such a steep incline in a distance of one hundred miles. It
is not, however, proposed to let the full force of the ocean in from
this end. The operation of flooding the Jordan valley would be commenced
at Haifa; from this point to the sea-level in the Ghor is only
twenty-five miles. The highest point in the plain of Esdraelon is one
hundred and fifty-seven feet above the sea. Through this it is proposed
to cut a canal two hundred feet wide and forty feet deep. The volume of
water thus let in, it is calculated, would be regulated to an inflow
which would equal about twenty Jordans, and, allowing for evaporation,
it is estimated that in five years the Dead Sea and the whole valley of
the Jordan would be submerged to the sea-level.
Public-domain text, read in full here on John Shaqi.
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