The geography and geology of south-eastern EgyptBall, John
Science
The geography and geology of south-eastern Egypt
Ball, John
Geology -- Egypt; Physical geography -- Egypt
to notice that Qash Amir (_Os_), (the “Scragged Hill” of the
Admiralty Chart), is in its turn quite distinct from Elba, Halaib
is called Elei,[19] and the Geziret Halaib is shown as a peninsula;
Kwolala is called “Geziret Elei,” and the Geziret el Dibia
(the Elba Island of the charts) is called Geziret Abu Fendira by
Schweinfurth. My Wadi Shellal he calls “Wadi Heberah,” and Cape
Elba (my Ras Hadarba) is noted as “Ras Edineb.” His “highest
peak” (South Peak of the charts) is Asotriba, the highest mountain
of the group, lying just within the Sudan; the name Asotriba
(Schweinfurth’s “Soturba”) means “green mountain,” and
refers to the vegetation on its slopes. Schweinfurth’s experience
of the Bisharin led him to give them a very bad character, though
he gives high recognition to their beauty of feature and figure;
but being unfamiliar with their language was, he admits, an obstacle
to forming a fair judgment of them.
In 1873, Colonels PURDY and COLSTON, two American officers attached
to the Egyptian Army, were commissioned by the Khedive Ismail Pasha
to carry out a reconnaissance for a proposed railway line between
Berenice and Berber. Colston[20] travelled overland from Qena _via_
Qoseir to Berenice, discovering several ancient stations on his
way to join Purdy. Though Purdy sanguinely states[21] that “la
construction d’un chemin de fer de ce point (Berenice) à Berber
n’offrirait pas de grandes difficultés,” the reconnaissance
appears to have been singularly rough for a decision in so weighty a
matter. Distances were mere guesses, and the only instruments employed
seem to have been a compass, aneroid, and hypsometer. The compass
must often have been unreliable owing to magnetic rocks, which in
places deflect the needle as much as 40° from its normal position,
while the use of the aneroid was so little understood that Purdy
could actually write, in the concluding paragraph of his paper: “Je
me permets de rappeler l’attention sur les notes barométriques
jointes à ce rapport. A ce propos, je dois faire observer que
quoique l’anéroïde soit très sensible aux changements de
niveau, il ne l’est pas assez pour la pression atmosphérique,
et sa marche est excessivement irrégulière. . . . Il m’est
arrivé, par exemple, de constater, le matin, au moment du départ,
une différence sensible du point marqué le soir précédent à
mon arrivée.” Not only are many of the place-names given by Purdy
erroneous, but some of his most important statements are contrary to
fact; to take only a few examples, the Wadi Kalalat is confused with
Wadi Shenshef, and Gebel Shut with Gebel Dahanib, while it is stated
that no water exists between Gebel Dif (_Fm_) and Gebel Egat (_Ft_),
although there are several good wells between the two places. The
map accompanying Purdy’s paper is full of errors, and almost
worse than useless. Of Colston’s route from Qena to Berenice there
was no published cartographic record until 1891, when G. CORA[22]
Public-domain text, read in full here on John Shaqi.
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