The journal of Frederick Horneman's travels, from Cairo to Mourzouk, the capital of the kingdom of Fezzan, in Africa, in the years 1797-8Hornemann, Friedrich
History
The journal of Frederick Horneman's travels, from Cairo to Mourzouk, the capital of the kingdom of Fezzan, in Africa, in the years 1797-8
Hornemann, Friedrich
Berber languages; Fezzan (Libya) -- Description and travel; Libyan Desert -- Description and travel
We reposed the rest of the day on this spot, distant from our last
encampment four hours march, and our chief dispatched a messenger to
Mourzouk, to give notice of arrival of the caravan on the frontier
of the kingdom, and to bear a letter of respect to the sultan from
each merchant individually.
And now, on the _sixteenth_, (dating by our departure from _Augila_),
we came again to the society of men: a march of nine hours bringing
us to _Temissa_, situated within the territory of Fezzan.
SECTION II.
_Observations on the Region of the Harutsch._
The mountainous desert of _Harutsch_ is the most remarkable region
that came within scope of my observation during this journey;
its extent has been stated to me at seven days journey over,
from north to south; and at five days from east to west: but in a
subsequent voyage from Fezzan to Tripoly, I fell in again with a
branch or tract of the _Harutsch_, and was there told, that it yet
extended further to the _west_. At Mourzouk, too, I was informed of
black mountains on the road leading southward to Bornou, on whose
heights the climate was of very cold temperature, and whence the
people of Mourzouk obtained their iron; and I conjecture that such
mountainous tract may be a further branch of the _Harutsch_, though
having indeed no positive information or proof of the immediate
junction or connection of these regions.
The rugged, broken, and altogether wild and terrific scene which
this desert tract affords, leads strongly to the supposition that its
surface at some period took its present convulsed form and appearance
from volcanic revolution. Its inequalities of ground are no where
of great altitude. The general face of country shews continued
ranges of hills, running in various directions, rising from eight
to twelve feet only above the level of the intermediate ground; and
between which branches, (on perfect flats, and without any gradual
ascent of base or fore-ground,) rise up lofty insulated mountains,
whose sides are exceeding steep from the very base. A mountain of
this description, situated midway on journey over this desert, and
north of our caravan road, is by the Arabs termed _Stres_; it has
the appearance of being split from the top down to the middle. I was
prevented from particular examination of it, but soon, on our caravan
halting, had the opportunity of inspecting another of the same kind.
Public-domain text, read in full here on John Shaqi.
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