The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
After having attained the highest point, or short table-land of the
Wadi-el-Araba, the descent in fact begins in a direct line nearly due
north to the Dead Sea; it is in places more elevated, rougher, and
more sandy than in others; and its width also becomes greater.
Gebel-el-Beianeh appears the _loftiest_ of the chain on the west; but
this is scarcely two-thirds as _high_ as the east range,
Gebel-el-Shera (_Mount Seir_); the former is entirely sterile and
arid, whilst the latter is covered with herbs and occasional trees,
and seems to have a sufficiency of rain. The east _Wadis_ also, which
are numerous, are filled with trees, shrubs, and flowers; and their
eastern and _higher_ portions, being well cultivated, yield good
crops. So Strabo, calling the district "Nabathæa," states it _abounded
in pastures_; hê Nabataia polyandros ousa hê chôra kai eubotos;[11]
and being the country of Esau, it was "of the fatness of the earth,
and of the dew of heaven from above."--_Gen._ xxvii. 39.
Footnote 11: _Strabo Geog._, vol. ii., lib. 16-35, p. 1103. Edit.
_Falconer_.
The range of Mount Seir, _Gebel-el-Shera_, _i.e._, the mountains of a
"region" or "tract," under which I have only included those mountains,
commencing with Mount _Seir_ itself on the north, and extending to
Gebel-el-Ithm on the south. On the eastern side is now _sandstone_,
veined with _oxide of iron_; and those mountains still further to the
east, forming a part of the Nabathæan chain, are _limestone_ with
_flints_, of the same _cretaceous_ series as that of the Sinaic
Peninsula; they present many varied forms and shapes.
El Araba, in the approach to Wadi Gharandel, is more covered with
shifting sands, broken by innumerable undulations, and low hills; into
these sands the waters of Wadi Gharandel, which, according to
Burckhardt, have a _sulphureous_ taste, lose themselves. In the ascent
of this Wadi (Gharandel) towards Gebel Kula, a mountain is climbed
which is composed of _calcareous_ rocks, _sandstone_ and _flints_,
lying over each other in horizontal layers. Gebel Kula is covered on
its summit, with a _chalky_ surface. But in Wadi Dalegheh the
mountains are _calcareous_, with some _flints_, and perfectly bare.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account