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
and 429.) Carl Zimmerman (in the learned Analysis of his “Karte von
Inner Asien,” 1841, S. 99) has made it appear extremely probable that
the Tarim depression, _i. e._ the desert between the mountain chains
of the Thian-schan and the Kuen-lün, where the Steppe river Tarim-gol
empties itself into the Lake of Lop, which used to be described as an
alpine lake, is hardly 1200 (1279 English) feet above the level of the
sea, or only twice the height of Prague. Sir Alexander Burnes also
assigns to that of Bokhara only an elevation of 1190 English feet. It
is earnestly to be desired, that all doubt respecting the elevation of
the plateaux of middle Asia, south of 45° of latitude, should finally
be set at rest by direct barometric measurements, or by determinations
of the boiling point of water made with more care than is usually given
to them. All our calculations respecting the difference between the
limits of perpetual snow, and the maximum elevation of vine cultivation
in different climates, rest at present on too complex and uncertain
elements.
In order to rectify in the smallest space that which was said in the
last edition of the present work, relatively to the great mountain
systems which intersect the interior of Asia, I subjoin the following
general review. We begin with the four parallel chains, which follow
with tolerable regularity an east and west direction, and are connected
with each other at a few detached points by transverse elevations.
Differences of direction indicate, as in the Alps of western Europe, a
difference in the epoch of elevation. After the four parallel chains
(the Altai, the Thian-schan, the Kuen-lün, and the Himalaya), we have
to notice chains following the direction of meridians, viz. the Ural,
the Bolor, the Khingan, and the Chinese chains, which, with the great
bend of the Thibetian and Assamo-Bermese Dzangbo-tschu, run north and
south. The Ural divides a part of Europe but little elevated above
the level of the sea from a part of Asia similarly circumstanced. The
latter was called by Herodotus, (ed. Schweighaüser, T. v. p. 204) and
even as early as Pherecydes of Syros, a Scythian or Siberian Europe,
including all the countries to the north of the Caspian and of the
Iaxartes; in this view it would be a continuation of Europe “prolonged
to the north of Asia.”
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