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
If there be, as Edrisi says, (page 7,) a water communication between
Kauga and Wangara, (no matter which way the water runs), the fact
of a common level, would, of course, be proved; and then it must
be admitted to be highly improbable, that any part of the course of
the White River, southward of Darfoor, should be on a lower level,
than the lake of Fittré. But, perhaps, some may doubt the authority
of Edrisi, in this point; and possibly, the more so, since he says,
that the Niger runs to the west.
But placing this circumstance out of the question, and leaving
the facts set forth by Mr. Browne and Mr. Horneman, to speak for
themselves, it may be asked,
1. Whether it is probable that the Niger, after running about 2250
British miles in direct distance from its source, should not have
arrived at a lower level, than that of the countries adjacent to
the heads of the Nile?[58]
2. Whether the course of the Misselâd river, from the south of
Darfoor, is not almost directly contrary to that which the Niger
should take from Wangara, in order to join the White River?
3. Whether the course of the waters, to the west of Darfoor, and of
the head of the White River, are not also reported to run _towards_
the quarter that contains the Niger, instead of _coming from it_? and
are they not said to run through a wet marshy country; whilst that
to the east, in the line between Fittré and the White River, is
high and mountainous?[59]
4. Has not the country of Wangara, &c. like that of Fittré,
the character of an alluvial tract, inundated by the periodical
floods of the Niger, to the extent of more than 350 British miles in
length, by more than 170 in breadth: and has not both that and Gana,
large fresh water lakes in the dry season?[60] May not so great an
extent of surface, suffice for the evaporation of the waters of
the Niger; as we have already an instance of the kind in Persia,
in which the _Heermend_, a river of more than 400 miles length of
course, is evaporated in less than ¹⁄₂₀ part of the surface
of the inundation formed in Wangara?[61] I now return to the general
geography.
Mr. Horneman, in describing the position of the southern states,
speaks of _Wadey_, bordering on the west of Darfoor; then _Metko_,
west, (or rather NW) of Wadey; both of which are watered by the
river which flows from Darfoor to the lake Fittré, (_i. e._
the _Misselâd_); and, finally, Fittré itself, to the NW of
Metko. Continuing the description—_Begarmé_[62] is said to lie N
of Wadey; Bournu, N of Fittré. _Bergoo_ seems not to have been known
to Horneman; or, perhaps, he may have confounded it with the Burgu
towards Augila (the _Berdoa_ of Delisle and D’Anville). Bergoo,
according to Mr. Browne, is an independent country: Metko and Wadey,
the same: so that the empire of Bournu ends with Fittré (or _Cooka_)
Margi, and Wangara, southward.[63]
Public-domain text, read in full here on John Shaqi.
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