Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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Raleigh First Made Known, In 1596, The System Of The
Mountains Of Parime, Between The Sources Of The Rio Carony
And the
Essequibo, by the name of Wacarima (Pacarima), and the Jesuits Acunha
and Artedia furnished, in 1639, the first
Precise notions of that part
of this system which extends from the meridian of Essequibo to that of
Oyapoc. There they place the mountains of Yguaracuru and Paraguaxo,
the former of which gives birth to a gold river (Rio de oro), a
tributary of the Curupatuba;* (* When we know that in Tamanac gold is
called caricuri; in Carib, caricura: in Peruvian, cori (curi), we
easily recognize in the names of the mountains and rivers
(Yguara-curu, Cura-patuba) which we have just marked, the indication
of auriferous soil. Such is the analogy of the imported roots in the
American tongues, which otherwise differ altogether from each other,
that 300 leagues west of the mountain Ygaracuru, on the banks of the
Caqueta, Pedro de Ursua heard of the province of Caricuri, rich in
gold washings. The Curupatuba falls into the Amazon near the Villa of
Monte Alegre, north-east of the mouth of the Rio Topayos.); and
according to the assertion of the natives, subterraneous noises are
sometimes heard from the latter. The ridge of this chain of mountains,
which runs in a direction south 85 degrees east from the peak of Duida
near the Esmeralda (latitude 3 degrees 19 minutes), to the rapids of
the Rio Manaye near Cape Nord (latitude 1 degree 50 minutes), divides,
in the parallel of 2 degrees, the northern sources of the Essequibo,
the Maroni and the Oyapoc, from the southern sources of the Rio
Trombetas, Curupatuba and Paru. The most southern spurs of this chain
approach nearer to the Amazon, at the distance of fifteen leagues.
These are the first heights which we perceived after having left
Xeberos and the mouth of the Huallaga. They are constantly seen in
navigating from the mouth of the Rio Topayo towards that of Paru, from
the town of Santarem to Almeirim. The peak Tripoupou is nearly in the
meridian of the former of those towns and is celebrated among the
Indians of Upper Maroni. It is said that farther eastward, at Melgaco,
the Serras do Velho and do Paru are still distinguished in the
horizon. The real boundaries of this series of sources of the Rio
Trombetas are better known southward than northward, where a
mountainous country appears to advance in Dutch and French Guiana, as
far as within twenty to twenty-five leagues of the coast. The numerous
cataracts of the rivers of Surinam, Maroni and Oyapoc, prove the
extent and the prolongation of rocky ridges; but in those regions
nothing indicates the existence of continued plains or table-lands
some hundred toises high, fitted for the cultivation of the plants of
the temperate zone.
The system of the mountains of Parime surpasses in extent nineteen
times that of the whole of Switzerland. Even considering the
mountainous group of the sources of the Rio Negro and the Xie as
independent or insulated amidst the plains, we still find the Sierra
Parime (between Maypures and the sources of the Oyapoc) to be 340
leagues in length; its greatest breadth (the rocks of Imataca, near
the delta of the Orinoco, at the sources of the Rio Paru) is 140
leagues.
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