The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850Various
Science
The Edinburgh New Philosophical Journal, Vol. XLIX: April-October 1850
Various
Science -- Periodicals
Captains Irby and Mangles, the _first_ Europeans who ascended Gebel
_Harun_, thus describe "the view from the summit." It "is extremely
extensive in every direction; but the eye rests on few objects which
it can clearly distinguish, and give a name to, although an excellent
idea is obtained of the general face and features of the country. The
chain of Idumean mountains, which form the western shore of the Dead
Sea, seem to run on to the south, though losing considerably in their
height. They appear in this point of view, barren and desolate. Below
them is spread out a white sandy plain, seamed with the beds of
occasional torrents, and presenting much the same features as the most
desert parts of the Ghor. Where this desert expanse approaches the
foot of Mount Hor, there arise out of it, like islands, several lower
peaks and ridges, of a purple colour, probably composed of the same
kind of _sandstone_ as that of Mount Hor itself, which, variegated as
it is in its hues, presents in the distance one uniform mass of dark
purple. Towards the Egyptian side there is an expanse of country
without features or limit, and lost in the distance. The lofty
district which we had quitted in our descent to Wadi Mousa, shuts up
the prospect on the south-east side; but there is no part of the
landscape which the eye wanders over with more curiosity and delight
than the crags of Mount Hor itself, which stand up on every side, in
the most rugged and fantastic forms, sometimes strangely piled one on
the other, and sometimes as strangely yawning in clefts of a frightful
depth."
Under the term _Nabathæan Chain_, or the chain of the mountains of
Edom, I have restricted those mountains beginning north of 30° N.
Lat., and which then tend round northward, by the east of Petra. They
are the loftiest on the east, attaining probably to an altitude of
3000 feet above the Wadi-el-Araba. This chain presents to the view, on
the east, long elevated ranges of _limestone_, sometimes with
_flints_, but of more easy slopes, _without_ precipices, being smooth
and rounded. Further still to the east, the high plateau of the Great
Eastern Desert--of which _El Nejd_ is a portion--stretches out to an
almost indefinite extent. To the west and north, and around Mount
_Hor_, lofty party-coloured _sandstone_ ridges and cliffs prevail;
then succeed high masses of _porphyry_, constituting the body of the
mountains, but _lower_ than the _sandstone_. And, lastly, more
northwards, the chain sinks down into low hills of _argillaceous_
rock, or of _limestone_.
The entire breadth of the _Seir_ range seems not to exceed eighteen
English miles, between Wadi-el-Araba and the Eastern Desert; whilst
that of the more northern, or _Nabathæan chain_, does not exceed
twenty-two miles between those districts.
Public-domain text, read in full here on John Shaqi.
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