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A dyke of granitic rocks crosses the Orinoco these rocks are, as it were, the columns of Hercules, beyond which no white man has been able to penetrate. It appears that this point, known by the name of the great Raudal de Guaharibos, is three-quarters of a degree west of Esmeralda, consequently in longitude 67 degrees 38 minutes.

We perceived no crocodiles in the raudal; these animals seem to shun the noise of cataracts. From Cabruta to the mouth of the Rio Sinaruco, a distance of nearly two degrees of latitude, the left bank of the Orinoco is entirely uninhabited; but to the west of the Raudal de Cariven an enterprising man, Don Felix Relinchon, had assembled some Jaruro and Ottomac Indians in a small village.

We were repeatedly assured that no one had ever been to the east of the Raudal of the Guaharibos; and that beyond that point, according to the opinion of some of the natives, the Orinoco descends like a small torrent from a group of mountains, inhabited by the Coroto Indians.

A range of shoals, that crosses almost the whole river, bears the name of the Raudal de Marimara. The river penetrates far into the land, and forms spacious bays in the rocks. In the evening the rocky coasts project their vast shadows over the surface of the river.

A little above the Cano Marapiche, which opens on the northern bank, a very long island divides the river into two branches. We passed on the south of this island without difficulty; northward, a chain of small rocks, half covered at high water, forms whirlpools and rapids. This is La Boca del Infierno, and the Raudal de Camiseta.

This passage is reputed to be dangerous when the water is very high; but we found the surface of the river beyond the raudal as smooth as glass. We passed the night in a rocky island called Piedra Raton, which is three-quarters of a league long, and displays that singular aspect of rising vegetation, those clusters of shrubs, scattered over a bare and rocky soil, of which we have often spoken.

When we again embarked on the Orinoco, we found the river free from shoals. After a few hours we passed the Raudal of Garcita, the rapids of which are easy of ascent, when the waters are high. To the eastward is seen a small chain of mountains called the chain of Cumadaminari, consisting of gneiss, and not of stratified granite.

I shall have occasion hereafter to mention the hypotheses that have given rise to these errors, in speaking of the source of the Orinoco. We stopped near the raudal of Cunuri. The noise of the little cataract augmented sensibly during the night, and our Indians asserted that it was a certain presage of rain.

Contiguous mountains are only found more to the east, towards the sources of the Pacimoni, Siapa, and Mavaca. Having arrived on the south of the Raudal of Caravine, we perceived that the Cassiquiare, by the windings of its course, again approached San Carlos.

The Indians remained rowing in the boat, without towing or pushing it forward with their arms, and wearying us with their wild cries. We passed the Canos of Uita and Endava on the west. It was night when we reached the Raudal de Tabaje.