The source of the Blue Nile : $b a record of a journey through the Soudan to Lake Tsana in western Abyssinia, and of the return to Egypt by the valley of the Atbara, with a note on the religion, customs, etc. of AbyssiniaHayes, Arthur J.
Religion
The source of the Blue Nile : $b a record of a journey through the Soudan to Lake Tsana in western Abyssinia, and of the return to Egypt by the valley of the Atbara, with a note on the religion, customs, etc. of Abyssinia
Hayes, Arthur J.
Ethiopia -- Description and travel; Ethiopia -- Religion; Sudan -- Description and travel
[Footnote 105: “Mittheilungen der Afrikanischen Gesellschaft
in Deutschland,” 1881, vol. iii. p. 28. The following general
description of the lake district embodied by Mr. Dupuis in his Report
on the Expedition, and published in Sir W. Garstin’s Despatch
already cited (Ed. 2165, 1904, p. 215), is terse and interesting:
“The depression occupied by the lake is, generally speaking,
saucer-shaped, the land rising from the edge of the water in gentle
undulating plains, getting steeper and steeper and terminating in
considerable hills or mountains of some importance. In several places,
as at Gorgora on the north, Mitraha and Koratsa on the east, Zegi
on the south, and Dengelber on the west, the hills come right down
to the lake and descend more or less abruptly into the water, but
more often they stand back at some distance from it. The geological
formation is almost everywhere of the same primitive character
that seems to be universal in the Eastern Soudan, granite, gneiss,
and quartz, varied only by tracts of lava, basalt, and eruptive
rocks. Sandstone is reported by some travellers, and lime-stone is
said to be found near Gondar, but I saw neither myself. The large
tracts of comparatively level land consist almost entirely of the
cracked black cotton soil usually found associated with igneous
rocks. At the mouths of all the larger rivers flowing into the lake
are extensive alluvial plains generally composed wholly of this same
cotton soil, and of the greatest fertility, though nine-tenths of
their area now grows nothing more valuable than coarse grass.”]
[Footnote 106: “Modern Abyssinia,” pp. 40-43.]
[Footnote 107: “Modern Abyssinia,” p. 42.]
[Footnote 108: _Adansonia digitata_. These are tall trees, whose
timber is of a spongy consistency. Sir S. Baker mentions one which
was about forty feet in circumference. He wrote: “The _Adansonia
digitata_, although a tree, always reminds me of a gigantic fungus;
the stem is disproportioned in its immense thickness to its height,
and its branches are few in number, and as massive in character
as the stem. The wood is not much firmer in substance than cork,
and is as succulent as a carrot.” (“The Nile Tributaries of
Abyssinia,” p. 356.)]
[Footnote 109: Governor.]
[Footnote 110: “If God is willing.”]
[Footnote 111: “The Nile Tributaries of Abyssinia,” pp. 124, 125.]
[Footnote 112: “Life in Abyssinia,” pp. 385, 386.]
[Footnote 113: “The Nile Tributaries of Abyssinia,” p. 240.]
[Footnote 114: This blight is known as “asal,” or “honey,”
from the sticky deposit formed all over the plant and leaves. At the
time of the expedition it prevailed more or less severely throughout
the greater part of the Kassala Moudirieh. The stalks of the plants
attacked become black.]
[Footnote 115: These are watertanks of galvanized iron. Two of them
form a camel’s load.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account