Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 1 (of 2)Werne, Ferdinand
History
Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 1 (of 2)
Werne, Ferdinand
Nile River
It is a strangely beautiful sight to see these exuberant plants,
sparkling in various colours, keeping down the more sturdy
ones. However, on our voyage back, the scene had so altered, that
it was with difficulty we could persuade ourselves that here it was
so wonderfully beautiful before. Together with the various species
of convolvulus, the blooming ambak-tree contributed to enhance the
variety of flowers. The Arabs call it ambak, although they are only
acquainted with its dry light wood, which floats down to them. The
tree grows only in the river itself, or in a swamp, and when the water
recedes, dies away to the root. The rapidity of its growth surpasses
that of the rising of the Nile, and shoots up from ten to fifteen feet
above its highest water-mark. It rises in a conical form out of the
water, but decreases again towards the root, and is, in the middle,
as thick as a strong man’s arm. The wood is throughout of a spongy
nature, and can be called only fibrous pith: it is overlaid with a
dark green rind, which is also furnished with a rough brownish hue
and small imperceptible arcuated thorns. The branches fix themselves
on luxuriant soil, like the acacias with us, and towards the ends
are quite green and rough; the leaves are twinned like those of the
acacia; the foliage is full of sap and green like reeds. The yellow
bean-flower grows single, but in great profusion; it is an inch and
a half long and broad, and has ten stamina round the pistil.
The top of a mountain, of which, at the moment, I could learn no other
name than that of Geb’l Dinka, rose, about nine o’clock, to the
S.S.W. This was a welcome sight to me, as it seemed to promise, from
the distance, something more magnificent than the hills, or would-be
mountains, that had hitherto appeared in the horizon. We make four
miles and a half, and the rapidity of the stream still remains one
mile, although the water before this Machada seems to have no fall,
and only to be set in motion by the pressure from above. At two
o’clock we had on the left, towards the east, Geb’l Dinka, so
termed by navigators, but more correctly called Geb’l N’jemati,
which is said to denote a group of mountain tops. Two rocky ridges
especially project, and seem to belong to the granite formation.
Public-domain text, read in full here on John Shaqi.
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