Aspects of nature, in different lands and different climates (Vol. 1 of 2): with scientific elucidationsHumboldt, Alexander von
Science
Aspects of nature, in different lands and different climates (Vol. 1 of 2): with scientific elucidations
Humboldt, Alexander von
Physical geography; Plant morphology; Science; South America -- Description and travel
Russegger’s scientific expedition,--which by Mehemet Ali’s desire
was sent to the gold-washings of Fazokl on the Blue (Green) Nile,
Bahr-el-Azrek, in 1837 and 1838,--had made the existence of the
“Mountains of the Moon” appear very doubtful. The Blue Nile, the
Astapus of Ptolemy, issuing from the lake of Coloe (now called lake
Tzana) winds from amongst the colossal Abyssinian mountains; but
towards the south-west an extensive low tract of country appears. The
three exploring expeditions sent by the Egyptian government, (one in
November 1839 from Chartum to the confluence of the Blue and the White
Nile, under the command of Selim Bimbashi; another in the autumn of
1840, which was accompanied by the French engineers Arnaud, Sabatier,
and Thibaud; and a third in August 1841), first unveiled the high
mountains which, between the parallels of 6°-4°, and probably still
farther to the south, run at first from west to east, and afterwards
from north-west to south-east, and approach the left bank of the
Bahr-el-Abiad. The second of Mehemet Ali’s expeditions first saw the
mountain chain, according to Werne’s account, in lat. 11-1/3° where
Gebel Abul and Gebel Kutak rise to 3400 (3623 Eng.) feet. The high land
continued and approached nearer to the river more to the south, between
4-3/4° lat., to the parallel of the island of Tschenker in 4° 4′, where
the expedition of Commander Selim and Feizulla Effendi terminated. The
shallow river makes its way between rocks, and detached mountains rise
again in the country of Bari to 3000 (3197 Eng.) feet. These probably
belong to the Mountains of the Moon as represented in our most recent
maps, although they are not indeed mountains covered with perpetual
snow such as Ptolemy had described (lib. iv. cap. 9). The limit of
perpetual snow in these latitudes would not certainly be found below
an elevation of 14500 (15450 Eng.) feet. Perhaps Ptolemy transferred
to the country of the sources of the White Nile the knowledge which
he may have had of the high mountains of Habesch, which are nearer to
Upper Egypt and to the Red Sea. In Godiam, Kaffa, Miecha, and Sami,
the Abyssinian mountains rise to 10000 and 14000 (10657 and 14920
Eng.) feet, according to exact measurements; not according to Bruce,
who gives the elevation of Chartum exceedingly wide of the truth,
_i. e._, 4730 (5041 Eng.) feet, instead of 1430 (1524 Eng.) feet!
Rüppell, one of the most accurate observers of the present day, found
Abba Jaret, in 13° 10′ of latitude, only 66 (70 Eng.) feet lower than
Mont Blanc. (Compare Rüppell, Reise in Abyssinien, Bd. i. S. 414, and
Bd. ii. S. 443). Rüppell found, adjoining the Buahat, an elevated
plain 13080 (13939 Eng.) feet above the Red Sea, barely covered with
a small quantity of fresh fallen snow (Humboldt, Asie Centrale, T.
iii. p. 272). The celebrated inscription of Adulis, which Niebuhr
considers to be somewhat later than Juba and than Augustus, also speaks
Public-domain text, read in full here on John Shaqi.
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