Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.
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But
It Is Different In The Missions Of Spanish Guiana, Where Nations Of
Various Races Are Mingled In The Village.
It is not even sufficient to
have learned the Caribee or Carina, the Guamo, the Guahive, the
Jaruro, the
Ottomac, the Maypure, the Salive, the Marivitan, the
Maquiritare, and the Guaica, ten dialects, of which there exist only
imperfect grammars, and which have less affinity with each other than
the Greek, German, and Persian languages.
The environs of the Mission of Carichana appeared to us to be
delightful. The little village is situated in one of those plains
covered with grass that separate all the links of the granitic
mountains, from Encaramada to beyond the Cataracts of Maypures. The
line of the forests is seen only in the distance. The horizon is
everywhere bounded by mountains, partly wooded and of a dark tint,
partly bare, with rocky summits gilded by the beams of the setting
sun. What gives a peculiar character to the scenery of this country
are banks of rock (laxas) nearly destitute of vegetation, and often
more than eight hundred feet in circumference, yet scarcely rising a
few inches above the surrounding savannahs. They now make a part of
the plain. We ask ourselves with surprise, whether some extraordinary
revolutions may have carried away the earth and plants; or whether the
granite nucleus of our planet shows itself bare, because the germs of
life are not yet developed on all its points. The same phenomenon
seems to be found also in the desert of Shamo, which separates
Mongolia from China. Those banks of solitary rock in the desert are
called tsy. I think they would be real table-lands, if the surrounding
plains were stripped of the sand and mould that cover them, and which
the waters have accumulated in the lowest places. On these stony flats
of Carichana we observed with interest the rising vegetation in the
different degrees of its development. We there found lichens cleaving
the rock, and collected in crusts more or less thick; little portions
of sand nourishing succulent plants; and lastly layers of black mould
deposited in the hollows, formed from the decay of roots and leaves,
and shaded by tufts of evergreen shrubs.
At the distance of two or three leagues from the Mission, we find, in
these plains intersected by granitic hills, a vegetation no less rich
than varied. On comparing the site of Carichana with that of all the
villages above the Great Cataracts, we are surprised at the facility
with which we traverse the country, without following the banks of the
rivers, or being stopped by the thickness of the forests. M. Bonpland
made several excursions on horseback, which furnished him with a rich
harvest of plants. I shall mention only the paraguatan, a magnificent
species of the macrocnemum, the bark of which yields a red dye;* (*
Macrocnemum tinctorium.) the guaricamo, with a poisonous root;* (*
Ityania coccidea.) the Jacaranda obtusifolia; and the serrape, or
jape* (* Dipterix odorata, Willd. or Baryosma tongo of Gaertner. The
jape furnishes Carichana with excellent timber.) of the Salive
Indians, which is the Coumarouna of Aublet, so celebrated throughout
Terra Firma for its aromatic fruit. This fruit, which at Caracas is
placed among linen, as in Europe it is in snuff, under the name of
tonca, or Tonquin bean, is regarded as poisonous. It is a false
notion, very general in the province of Cumana, that the excellent
liqueur fabricated at Martinique owes its peculiar flavour to the
jape. In the Missions it is called simaruba; a name that may occasion
serious mistakes, the true simaruba being a febrifuge species of the
Quassia genus, found in Spanish Guiana only in the valley of Rio
Caura, where the Paudacot Indians give it the name of achecchari.
I found the dip of the magnetic needle, in the great square at
Carichana, 33.7 degrees (new division). The intensity of the magnetic
action was expressed by two hundred and twenty-seven oscillations in
ten minutes of time; an increase of force that would seem to indicate
some local attraction. Yet the blocks of the granite, blackened by the
waters of the Orinoco, have no perceptible action upon the needle.
The river had risen several inches during the day on the 10th of
April; this phenomenon surprised the natives so much the more, as the
first swellings are almost imperceptible, and are usually followed in
the month of April by a fall for some days. The Orinoco was already
three feet higher than the level of the lowest waters. The natives
showed us on a granite wall the traces of the great rise of the waters
of late years. We found them to be forty-two feet high, which is
double the mean rise of the Nile. But this measure was taken in a
place where the bed of the Orinoco is singularly hemmed in by rocks,
and I could only notice the marks shown me by the natives. It may
easily be conceived that the effect and the height of the increase
differs according to the profile of the river, the nature of the banks
more or less elevated, the number of rivers flowing in that collect
the pluvial waters, and the length of ground passed over. It is an
unquestionable fact that at Carichana, at San Borja, at Atures, and at
Maypures, wherever the river has forced its way through the mountains,
you see at a hundred, sometimes at a hundred and thirty feet, above
the highest present swell of the river, black bands and erosions, that
indicate the ancient levels of the waters. Is then this river, which
appears to us so grand and so majestic, only the feeble remains of
those immense currents of fresh water which heretofore traversed the
country at the east of the Andes, like arms of inland seas? What must
have been the state of those low countries of Guiana that now undergo
the effects of annual inundations? What immense numbers of crocodiles,
manatees, and boas must have inhabited these vast spaces of land,
converted alternately into marshes of stagnant water, and into barren
and fissured plains!
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