Views of nature: or Contemplations on the sublime phenomena of creation: with scientific illustrationsHumboldt, Alexander von
Science
Views of nature: or Contemplations on the sublime phenomena of creation: with scientific illustrations
Humboldt, Alexander von
Physical geography; Plant morphology; Science; South America -- Description and travel
The Sorata and Illimani were first measured by the distinguished
geologist, Pentland, in the years 1827 and 1838; and since the
publication of his large map of the basin of the Laguna de Titicaca,
in June, 1848, we learn that the above elevations given for the Sorata
and Illimani are 3960 feet and 2851 feet too high. His map gives only
21,286 feet for the Sorata, and 21,149 feet for the Illimani. A more
exact calculation of the trigonometrical operations of 1838 led Mr.
Pentland to these new results. He ascribes an elevation of from 21,700
to 22,350 feet to four summits of the western Cordilleras; and,
according to his data, the Peak of Sahama would thus be 926 feet
higher than the Chimborazo, but 850 feet lower than the Peak of
Aconcagua.
Footnote 6:
p. 2—“_The desert near the basaltic mountains of Harudsch_.”
Near the Egyptian Natron Lakes, which in Strabo’s time had not yet
been divided into the six reservoirs by which they are now
characterized, there rises abruptly to the north a chain of hills,
running from east to west past Fezzan, where it at length appears to
form one connected range with the Atlas chain. It divides in
north-eastern, as Mount Atlas does in north-western Africa the Lybia,
described by Herodotus as inhabited and situated near the sea, from
the land of the Berbirs, or Biledulgerid, famed for the abundance of
its wild animals. On the borders of Middle Egypt the whole region,
south of the 30th degree of latitude, is an ocean of sand, studded
here and there with islands or oases abounding in springs and rich in
vegetation. Owing to the discoveries of recent travellers, a vast
addition has been made to the number of the Oases formerly known, and
which the ancients limited to three, compared by Strabo to spots upon
a panther’s skin. The third Oasis of the ancients, now called Siwah,
was the _nomos_ of Ammon, a hierarchical seat and a resting-place for
the caravans, which inclosed within its precincts the temple of the
horned Ammon and the spring of the Sun, whose waters were supposed to
become cool at certain periods. The ruins of Ummibida (_Omm-Beydah_)
incontestably belong to the fortified caravanserai at the Temple of
Ammon, and therefore constitute one of the most ancient monuments
which have come down to us from the dawn of human civilization.[AG]
The word Oasis is Egyptian, and is synonymous with Auasis and
Hyasis.[AH] Abulfeda calls the Oases _el-Wah_. In the latter time of
the Cæsars, malefactors were sent to the Oases, being banished to
these islands in the sandy ocean, as the Spaniards and English
transported their malefactors to the Falkland islands and New Holland.
The ocean affords almost a better chance of escape than the desert
surrounding the Oases; which, moreover, diminish in fruitfulness in
proportion to the greater quantity of sand incorporated in the soil.
Public-domain text, read in full here on John Shaqi.
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