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4<br />

going to relate will serve to elucidate the theory of volcanic reactions, or the influence of a system of<br />

volcanoes on a vast space of circumjacent country.<br />

At the time that Mr. Bonpland and myself inhabited the provinces of New Andalusia, Nueva-<br />

Barcelona, and Caraccas, a general opinion prevailed, that the easternmost parts of these coasts were the<br />

most exposed to the destructive effects of earthquakes. The inhabitants of Cumana dreaded the valley of<br />

Caraccas, on account of its damp and variable climate, and its gloomy and foggy sky; while the<br />

inhabitants of that temperate valley considered Cumana as a town, where only a burning air was breathed,<br />

and where the soil is periodically agitated by violent commotions. Forgetful of the overthrow of<br />

Riobamba, and other very elevated towns; ignorant that the peninsula of Araya, composed of mica-slate,<br />

has partaken of the commotions of the calcareous coast of Cumana; well-informed persons thought they<br />

perceived motives of security in the structure of the primitive rocks of Caraccas, as well as in the elevated<br />

situation of this valley. Religious ceremonies celebrated at La Guayra, and even in the capital, in the<br />

middle of the night*, recalled no doubt to their memory,<br />

* For instance, the nocturnal procession of the 21st of October, instituted in commemoration of the<br />

great earthquake,

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