The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
Next, turning to the north down the narrow declivity called _Nakb
Hawi_, the "windy pass," of which the stupendous _granite_ walls or
cliffs elevate themselves to about 800 feet, passing to the west end
of _Wadi Solaf_, where it meets _Wadi Firan_ and _Wadi-el-Sheikh_, and
following the last valley as far as _El Szaleib_, that ascent is
attained. There the formation consists of _granite_, on the upper beds
of which run layers of _red felspar_. North-east of _Wadi-el-Ush_ is
situate _Gebel Sheyger_, which affords some native _cinnabar_. The
three principal passes leading from the sandy Debbet-el-Ramleh on to
the great desert over the Tyh range, are, _El Mureikhi_ near the
centre and near _Gebel-el-Egmeh_; then _El Warsah_, said to be of too
rapid an ascent for caravans; and the third, which is most to the
west, _El Rakineh_ (the painted.) Afterwards, at some distance to the
NW., is the valley opening past _Ras Wadi Gharandel_, that has already
been described.
Proceeding, again, across the plain El Ramleh, and over the pass
Mureikhi on to the Desert-el-Tyh, in the approach to the castle of
_Nakhl_, on the east, a few miles off, low _chalky_ hills appeared;
and in places there were holes wherein _rock-salt_ had been dug. The
water at Nakhl is brackish, and the ground chalky, covered with loose
pebbles. _Wadi Nesil_ was observed to be overgrown with green shrubs.
_Gebel-el-Thughar_, signifying "the mouths," presents a mountainous
tract, in which followed a valley with _calcareous_ hills: here deep
sands were lodged, and large insulated rocks of a porous _tufa_,
called by Burckhardt _tufwacke_, lie scattered in many places.
"The termination of the vast gravelly plain we had been crossing
from _Nakhl_ was now at hand; but we could yet see it spreading
out wide to our left, the mirage giving its distant portions the
appearance of a succession of blue lakes; directly in front were
the mountains which close it in; and far to the right we could
see, stretching away, a still higher range running to the north,
and on the left the tops of the mountains about Wadi Gharandel,
the _Taset_ (cup) _Soddur_ being conspicuous afar. We entered
these mountains by a slight ascent, which struck soon after the
head of a long winding valley descending towards Suez: the immense
plain we had traversed, floated away in mist, and we had now done
with the plateau of the Great Desert."[15]
Footnote 15: _Bartlett's_ "Forty Days in the Desert," p. 167.
Thence a plain, which is below the level of the Desert-el-Tyh, and
covered with moving _sands_, extends as far as the sea-shore. These
_sands_ are collected by the winds, in many spots, into hills 30 or 40
feet high. The wells at _Mabuk_ afford good water by digging to the
depth of 10 or 12 feet.
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account