The historians' history of the world in twenty-five volumes, volume 02 : $b Israel, India, Persia, Phoenicia, Minor Nations of Western Asia
History
The historians' history of the world in twenty-five volumes, volume 02 : $b Israel, India, Persia, Phoenicia, Minor Nations of Western Asia
World history
The Jordan first traverses a small lake, which is almost dry in summer,
and then flows into the lake of Gennesareth or Tiberias, also called
the Sea of Galilee, and famous in Christian tradition. The shape of
this lake is an irregular oval, twenty kilometres in length by about
nine in breadth. The water is fresh and fit for drinking, but the
volcanic nature of the soil is indicated by springs of hot water in the
vicinity, and by the basaltic rocks that cover its shores. Its level is
two hundred and thirty metres below that of the sea. This low level has
been found constant throughout the whole valley of the Jordan, which,
leaving the lake of Gennesareth, continues its course southwards, and,
at a distance of twenty-five leagues from it, falls into the Dead Sea.
The mouth is four hundred metres below the level of the Mediterranean.
The Dead Sea, also called Lake Asphaltites, because of the bitumen
which floats upon its surface, is a lake with no outlet, and loses by
evaporation about the same amount of water that it receives from the
Jordan and its other affluents. It is sixty-four kilometres in length,
its breadth varies from eight to thirteen kilometres, its greatest
depth is about four hundred metres. Its basin is the bottom of the
great valley which extends from Mount Hermon to the Gulf of Akabah on
the Red Sea. This basin is in all likelihood due to the giving way of
a vast crater formed by the great volcanic eruption which swallowed
up the cities of Pentapolis. Genesis has preserved the memory of
this cataclysm, which it calls a rain of fire and brimstone. In the
neighbourhood we find deposits of lava, pumice-stone, sulphur, and
bitumen. The saltness and causticity of the water of the Dead Sea
explain why no fish nor any sort of animal can live in it; it contains
twenty-four to twenty-six and a quarter per cent. of saline matter,
in place of the four per cent. of other seas. Its specific gravity
is greater by a fifth than that of the water of the ocean, and it is
consequently impossible to drown in it. The saline concretions met with
in such regions as this may have given rise to the fable of Lot’s wife,
who was changed into a pillar of salt.
Public-domain text, read in full here on John Shaqi.
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