Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
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We In Vain Hoped
To Find On The Mountains Of Caracas, And Subsequently On The Back
Of The Andes, An Eglantine Near These Brambles.
We did not find one
indigenous rose-tree in all South America, notwithstanding the
analogy existing between the climates of the high mountains of the
torrid zone and the climate of our temperate zone.
It appears that
this charming shrub is wanting in all the southern hemisphere,
within and beyond the tropics. It was only on the Mexican mountains
that we were fortunate enough to discover, in the nineteenth degree
of latitude, American eglantines.* (* M. Redoute, in his superb
work on rose-trees, has given our Mexican eglantine, under the name
of Rosier de Montezuma, Montezuma rose.)
We were sometimes so enveloped in mist, that we could not, without
difficulty, find our way. At this height there is no path, and we
were obliged to climb with our hands, when our feet failed us, on
the steep and slippery acclivity. A vein filled with porcelain-clay
attracted our attention.* (* The breadth of the vein is three feet.
This porcelain-clay, when moistened, readily absorbs oxygen from
the atmosphere. I found, at Caracas, the residual nitrogen very
slightly mingled with carbonic acid, though the experiment was made
in phials with ground-glass stoppers, not filled with water.) It is
of snowy whiteness, and is no doubt the remains of a decomposed
feldspar. I forwarded a considerable portion of it to the intendant
of the province. In a country where fuel is not scarce, a mixture
of refractory earths may be useful, to improve the earthenware, and
even the bricks. Every time that the clouds surrounded us, the
thermometer sunk as low as 12 degrees (to 9.6 degrees R.); with a
serene sky it rose to 21 degrees. These observations were made in
the shade. But it is difficult, on such rapid declivities, covered
with a dry, shining, yellow turf, to avoid the effects of radiant
heat. We were at nine hundred and forty toises of elevation; and
yet at the same height, towards the east, we perceived in a ravine,
not merely a few solitary palm-trees, but a whole grove. It was the
palma real; probably a species of the genus Oreodoxa. This group of
palms, at so considerable an elevation, formed a striking contrast
with the willows* scattered on the depth of the more temperate
valley of Caracas. (* Salix Humboldtiana of Willdenouw. On the
alpine palm-trees, see my Prolegomena de Dist. Plant. page 235.) We
here discovered plants of European forms, situated below those of
the torrid zone.
After proceeding for the space of four hours across the savannahs,
we entered into a little wood composed of shrubs and small trees,
called el Pejual; doubtless from the great abundance here of the
pejoa (Gaultheria odorata), a plant with very odoriferous leaves.*
(* It is a great advantage of the Spanish language, and a
peculiarity which it shares in common with the Latin, that, from
the name of a tree, may be derived a word designating an
association or group of trees of the same species. Thus are formed
the words olivar, robledar, and pinal, from olivo, roble, and pino.
The Hispano-Americans have added tunal, pejual, guayaval, etc.,
places where a great many Cactuses, Gualtheria odoratas, and
Psidiums, grow together.) The steepness of the mountain became less
considerable, and we felt an indescribable pleasure in examining
the plants of this region. Nowhere, perhaps, can be found collected
together, in so small a space, productions so beautiful, and so
remarkable in regard to the geography of plants. At the height of a
thousand toises, the lofty savannahs of the hills terminate in a
zone of shrubs which, by their appearance, their tortuous branches,
their stiff leaves, and the magnitude and beauty of their purple
flowers, remind us of what is called, in the Cordilleras of the
Andes, the vegetation of the paramos and the punas.* (* For the
explanation of these words, see above Chapter 1.5.) We there find
the family of the alpine rhododendrons, the thibaudias, the
andromedas, the vacciniums, and those befarias with resinous
leaves, which we have several times compared to the rhododendron of
our European Alps.
Even when nature does not produce the same species in analogous
climates, either in the plains of isothermal parallels,* (We may
compare together either latitudes which in the same hemisphere
present the same mean temperature (as, for instance, Pennsylvania
and the central part of France, Chile and the southern part of New
Holland); or we may consider the relations that may exist between
the vegetation of the two hemispheres under isothermal parallels.)
or on table-lands, the temperature of which resembles that of
places nearer the poles,* we still remark a striking resemblance of
appearance and physiognomy in the vegetation of the most distant
countries. (* The geography of plants comprises not merely an
examination of the analogies observed in the same hemisphere; as
between the vegetation of the Pyrenees and that of the Scandinavian
plains; or between that of the Cordilleras of Peru and of the
coasts of Chile. It also investigates the relations between the
alpine plants of both hemispheres. It compares the vegetation of
the Alleghanies and the Cordilleras of Mexico, with that of the
mountains of Chile and Brazil. Bearing in mind that every
isothermal line has an alpine branch (as, for instance, that which
connects Upsala with a point in the Swiss Alps), the great problem
of the analogy of vegetable forms may be defined as follows: 1st,
examining in each hemisphere, and at the level of the coasts, the
vegetation on the same isothermal line, especially near convex or
concave summits; 2nd, comparing, with respect to the form of
plants, on the same isothermal line north and south of the equator,
the alpine branch with that traced in the plains; 3rd, comparing
the vegetation on homonymous isothermal lines in the two
hemispheres, either in the low regions, or in the alpine regions.)
This phenomenon is one of the most curious in the history of
organic forms.
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