Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.


































































































































 -  (* The
chego (Pulex penetrans) which penetrates under the nails of the toe in
men and monkeys, and there deposits its - Page 138
Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland. - Page 138 of 406 - First - Home

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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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