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
Chego (Pulex Penetrans) Which Penetrates Under The Nails Of The Toe In
Men And Monkeys, And There Deposits Its
Eggs.) It is now entirely
deserted, while opposite to it, on the right bank of the river, the
little mountains
Of Coruato are the retreat of wandering Indians,
expelled either from the Missions, or from tribes that are not subject
to the government of the monks.
Struck with the extreme breadth of the Orinoco, between the mouth of
the Apure and the rock Curiquima, I ascertained it by means of a base
measured twice on the western beach. The bed of the Orinoco, at low
water, was 1906 toises broad; but this breadth increases to 5517
toises, when, in the rainy season, the rock Curiquima, and the farm of
Capuchino near the hill of Pocopocori, become islands. The swelling of
the Orinoco is augmented by the impulse of the waters of the Apure,
which, far from forming, like other rivers, an acute angle with the
upper part of that into which it flows, meets it at right angles.
We first proceeded south-west, as far as the shore inhabited by the
Guaricoto Indians on the left bank of the Orinoco, and then we
advanced straight toward the south. The river is so broad that the
mountains of Encaramada appear to rise from the water, as if seen
above the horizon of the sea. They form a continued chain from east to
west. These mountains are composed of enormous blocks of granite,
cleft and piled one upon another. Their division into blocks is the
effect of decomposition. What contributes above all to embellish the
scene at Encaramada is the luxuriance of vegetation that covers the
sides of the rocks, leaving bare only their rounded summits. They look
like ancient ruins rising in the midst of a forest. The mountain
immediately at the back of the Mission, the Tepupano* of the Tamanac
Indians is terminated by three enormous granitic cylinders, two of
which are inclined, while the third, though worn at its base, and more
than eighty feet high, has preserved a vertical position. (*
Tepu-pano, place of stones, in which we recognize tepu stone, rock, as
in tepu-iri, mountain. We here perceive that Lesgian Oigour-Tartar
root tep, stone (found in America among the Americans, in teptl; among
the Caribs, in tebou; among the Tamanacs, in tepuiri); a striking
analogy between the languages of Caucasus and Upper Asia and those of
the banks of the Orinoco.) This rock, which calls to mind the form of
the Schnarcher in the Hartz mountains, or that of the Organs of
Actopan in Mexico,* composed formerly a part of the rounded summit of
the mountain. (* In Captain Tuckey's Voyage on the river Congo, we
find represented a granitic rock, Taddi Enzazi, which bears a striking
resemblance to the mountain of Encaramada.) In every climate,
unstratified granite separates by decomposition into blocks of
prismatic, cylindric, or columnar figures.
Opposite the shore of the Guaricotos, we drew near another heap of
rocks, which is very low, and three or four toises long.
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