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and on the banks of the Casanare, the Meta, the Oroonoko, and the Ventuario. Father Gili* has described
these commotions in a country entirely granitic, at the mission of Encaramada, where they were
accompanied by loud explosions. Great fallings in of the earth took place in the mountain Paurari; and
near the rock Aravacoto a small island disappeared in the Oroonoko. The undulatory motion continued
during a whole hour. This seemed the first signal of those violent commotions, which shook the coasts of
Cumana and Cariaco for more than ten months. It might be supposed, that men scattered in woods, with
no other shelter than huts of reeds and palm-leaves, had nothing to dread from earthquakes; but they
terrify the Indians of Erevato and Caura, as a phenomenon that seldom happens, frightens the beasts of
the forests, and impels the crocodiles to quit the depth of the waters for the shore. Nearer the sea, where
the shocks are frequent, far from being dreaded by the inhabitants, they are regarded with satisfaction as
the prognostics of a wet and fertile year.
In this dissertation on the earthquakes of Terra Firma and on the volcanoes of the neighbouring
Archipelago of the West India islands, I have pursued the general plan adopted in this
* Saggio di Storia Americana, vol. ii, p. 6.