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 — John Shaqi
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
This mountain I perceived, from the foot to the summit, to be covered
with detached stones, such as wholly constitute the lower hills. The
small plain from which this mountain rose, was encompassed by rows
of hills, such as above described, closely running into each other,
and connected as a wall. The flat within was overspread with white
quicksand, on which lay, irregularly scattered, large blocks of
stone, of like nature and substance as that generally throughout
this desert. With some trouble I procured a sample of the earthy
stratum beneath the sand: it seemed to me, at the time, to have the
appearance of ashes thrown out from a volcano; but I have since
lost the paper which contained the specimen, and cannot further
confirm the accuracy of my first observation. In the vicinity of
this mountain, I found stones of smaller bulk and a reddish colour,
resembling that of burnt bricks; some of these were one-half red,
the other blackish; the red part had not the same weight or density,
on fracture, as the black: the former is more porous and spongy,
and bears a general resemblance to slags or scoriæ.
The stony substance, of which the mass of these mountains consists,
varies in colour and density; in some parts heavy and compact, in
others having small holes and cavities. These species of stone are
intermingled, and I could not discover in either, any extraneous
matter or substance.
The stratification or lay of these stones is perfectly horizontal, but
often disturbed; parts of the first layer sinking into and mixing with
the second below, and the second with the third. Sometimes the strata
take an oblique direction; sometimes are promiscuously confused,
and sometimes no strata appear at all; and a series of low hills
is formed of one solid mass of rock, with fissures in direction to
the north. The plain too shews occasionally level rock of the like
nature and substance, in parts where bare of sand or soil. The whole
of this region of hillocks, hills, rocks, and mountains, is, in parts,
intersected by vales, occasionally having water; and though the soil
is of white sand, yet it is so far fertile as to produce single trees,
and pasturage for beasts; in these productive spots are frequently
to be seen the tracks and slots of game. Often, when I thought I
could so do without danger of losing my way, I struck into one of the
narrow vales running apparently in the same direction as our caravan
road; and occasionally led away to defiles becoming more narrow and
rugged, I repented my indiscretion, whilst thus separated from my
company, and exposed to attack from Bedouins, with dependence for
safety on my single sabre and pistols. On regaining the caravan,
it yet occurred that my danger had not been great, for what Arab
robber could look for a traveller in such a tract, or suppose any
hardy enough to wander therein from his troop, excepting, indeed,
some wretched Moroccan pilgrim in search of water!
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