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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The Rivers That Rise On The Eastern Declivity Of The Andes
(For Instance The Napo) Carry Along With Them A Great Deal Of Gold,
Even When Their Sources Are Found In Trachytic Soils.
Why may there
not be an alluvial auriferous soil to the east of the Cordilleras, as
there is to the west, in the Sonoro, at Choco, and at Barbacoas?
I am
far from wishing to exaggerate the riches of this soil; but I do not
think myself authorized to deny the existence of precious metals in
the primitive mountains of Guiana, merely because in our journey
through that country we saw no metallic veins. It is somewhat
remarkable that the natives of the Orinoco have a name in their
languages for gold (carucuru in Caribbee, caricuri in Tamanac, cavitta
in Maypure), while the word they use to denote silver, prata, is
manifestly borrowed from the Spanish.* (* The Parecas say, instead of
prata, rata. It is the Castilian word plata ill-pronounced. Near the
Yurubesh there is another inconsiderable tributary stream of the Rio
Negro, the Curicur-iari. It is easy to recognize in this name the
Caribbee word carucur, gold. The Caribs extended their incursions from
the mouth of the Orinoco south-west toward the Rio Negro; and it was
this restless people who carried the fable of El Dorado, by the same
way, but in an opposite direction (from south-west to north-east),
from the Mesopotamia between the Rio Negro and the Jupura to the
sources of the Rio Branco.) The notions collected by Acunha, Father
Fritz, and La Condamine, on the gold-washings south and north of the
river Uaupe, agree with what I learnt of the auriferous soil of those
countries. However great we may suppose the communications that took
place between the nations of the Orinoco before the arrival of
Europeans, they certainly did not draw their gold from the eastern
declivity of the Cordilleras. This declivity is poor in mines,
particularly in mines anciently worked; it is almost entirely composed
of volcanic rocks in the provinces of Popayan, Pasto, and Quito. The
gold of Guiana probably came from the country east of the Andes. In
our days a lump of gold has been found in a ravine near the mission of
Encaramada, and we must not be surprised if, since Europeans settled
in these wild spots, we hear less of the plates of gold, gold-dust,
and amulets of jade-stone, which could heretofore be obtained from the
Caribs and other wandering nations by barter. The precious metals,
never very abundant on the banks of the Orinoco, the Rio Negro, and
the Amazon, disappeared almost entirely when the system of the
missions caused the distant communications between the natives to
cease.
The banks of the Upper Guainia in general abound much less in
fishing-birds than those of Cassiquiare, the Meta, and the Arauca,
where ornithologists would find sufficient to enrich immensely the
collections of Europe. This scarcity of animals arises, no doubt, from
the want of shoals and flat shores, as well as from the quality of the
black waters, which (on account of their very purity) furnish less
aliment to aquatic insects and fish.
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