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Updated: June 3, 2025
The araguato of Caripe is a new species of the genus Stentor, which I have above described. Its eye, voice, and gait, denote melancholy. I have seen young araguatoes brought up in Indian huts. They never play like the little sagoins, and their gravity was described with much simplicity by Lopez de Gomara, in the beginning of the sixteenth century.
As we approach those periods in which organic life develops itself in a greater number of forms, the phenomenon of grottoes becomes more frequent. It is this rock which so often interrupts the course of rivers, by engulfing them into its bosom. In this also is formed the famous Cueva del Guacharo, and the other grottoes of the valley of Caripe.
Northward the granitic chain of the Silla de Caracas and Porto Cabello are separated from the Llanos by a screen of mountains that are schistose between Villa de Cura and Parapara, and calcareous between the Bergantin and Caripe. I was no less struck by this absence of blocks on the banks of the Amazon.
Their sprightliness diminishes, as their intellectual faculties appear to increase. We stopped to observe some howling monkeys, which, to the number of thirty or forty, crossed the road, passing in a file from one tree to another over the horizontal and intersecting branches. While we were observing their movements, we saw a troop of Indians going towards the mountains of Caripe.
Notwithstanding the inconsiderable elevation of the mountains of Cumana, the descent is extremely difficult and dangerous in the direction of Cariaco. The Cerro of Santa Maria, which the missionaries ascend in their journey from Cumana to their convent at Caripe, is famous for the difficulties it presents to travellers.
The only petrifactions of shells which I found in this limestone formation consist of a heap of turbinites and trochites, on the flank of Turimiquiri, at more than 680 toises high, and an ammonite seven inches in diameter, in the Montana de Santa Maria, north-north-west of Caripe.
Descending the Cuchillo de Guanaguana towards the convent of Caripe, we find another more recent formation, white, with a smooth or slightly conchoidal fracture, and divided in very thin layers, which succeeds to the bluish grey limestone formation of Cumanacoa.
In another part of South America, near the town of Cumana, is a vast cavern in the Valley of Caripe, which was many years ago visited by Baron Humboldt, who found it inhabited by a remarkable species of nocturnal bird, called the guacharo. The mouth of the cavern is pierced in the side of the cliff looking towards the south, in the form of an arch, eighty feet wide and seventy-two in height.
During my stay in America I took the limestone of Cumanacoa for zechstein or Alpine limestone, and that of Caripe for Jura limestone. There is in Venezuela a suppression of the different strata which, in the old continent, separate zechstein from Jura limestone.
The Guacharos alone would have been sufficient to render it celebrated. These nocturnal birds have been nowhere yet discovered except in the mountains of Caripe and Cumanacoa. But his account of Caripe was fully corroborated by my host, who had gone there last year, and, by the help of the magnesium light, had penetrated farther into the cave than either the bishop or Humboldt.
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