Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 2 (of 2)Werne, Ferdinand
History
Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 2 (of 2)
Werne, Ferdinand
Nile River
A quarter before one. From E. by N. A gohr on the right, and we go,
at one o’clock, E.S.E. Half-past one. The river takes a direction
before us to E., with some little inlets, so that we cannot see the
lower shore. The wind blows strongly against us from E. We have but
scanty fare, being without meat. I cannot deny _kew_ to myself now,
for I really want it.
Half-past two. E. by S. A Haba on the right, before it a lake
connected with the river in front; the forest is upon a gentle
declivity, and covered with shrubs, thorns, and dwarf-trees, even to
the edge of the water. The shore also falls away gently to the river,
near which it only rises a little above the narrow green margin of
grass. We halt close to the right shore, owing to want of wood.
The shore ascends to about fifteen feet high, where the trees begin,
and is composed of nothing but mimosas, although the Nile very
certainly does not flow over it; for the river has full play far
away to the left.
If we call these lakes, marshes, and reed-morasses, a longitudinal
valley, enclosed as they are with the Nile between two high shores,
which, however, do not ascend to the due height, the original shores
perhaps lying still further by the irregular low line of mountains,
or rather hills, it is plain that the same is gradually filled by
alluvial deposits from the mountains of Bari, or from above, and an
accumulation of vegetables, or the momentary sprouting forth of an
corresponding kingdom of plants, must have soon followed the more
important vegetable matter. As the sluices of the so-called valley
pour into the great Nile, it must have falls on a level with the Nile
itself, and has, therefore, dug a bed, and made an even slope to this
side, after the stream had removed the first barriers or dikes of the
high shores, which are now secure from any inundation. A river-bed,
indeed, naturally becomes deeper when there is a proper fall and a
regular conduit. The lower Nile has elevated its bed, because it has
but few vents. Why could not the White River have a similar retrograde
connection of water, which is prevented from flowing off, such as is
the case, in the first place, near Khartùm? The Nile here might have
been previously in majestic fullness, and flowed rapidly between the
present old shores to Khartùm, until it created shallows and islands,
where reeds and water-plants of every species sprang forth luxuriantly
from the nearly stagnant water, and vehemently opposed the natural
course of the river, seized the alluvial deposits from above in their
polypi-arms, and rose to what we now see to be meadows and marshes.
Public-domain text, read in full here on John Shaqi.
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