Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
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I Never Could Have Pronounced The Opinion, That The Silla And The
Cerro De Avila, Mountains Of Gneiss And Mica-Slate, Were In
Dangerous Proximity To The City Of Caracas Because They Contained A
Great Quantity Of Pyrites In Subordinate Beds Of Primitive
Limestone.
But I remember having said, during my stay at Caracas,
that the eastern extremity of Terra Firma appeared, since the great
earthquake of Quito, in a state of agitation, which warranted
apprehension that the province of Venezuela would gradually be
exposed to violent commotions.
I added, that when a country had
been long subject to frequent shocks, new subterranean
communications seemed to open with neighbouring countries; and that
the volcanoes of the West India Islands, lying in the direction of
the Silla, north-east of the city, were perhaps the vents, at the
time of an eruption, for those elastic fluids which cause
earthquakes on the coasts of the continent. These considerations,
founded on local knowledge of the place, and on simple analogies,
are very far from a prediction justified by the course of physical
events.
On the 30th of April, 1812, whilst violent commotions were felt
simultaneously in the valley of the Mississippi, in the island of
St. Vincent, and in the province of Venezuela, a subterranean noise
resembling frequent discharges of large cannon was heard at
Caracas, at Calabozo (situated in the midst of the steppes), and on
the borders of the Rio Apure, over a superficies of four thousand
square leagues. This noise began at two in the morning.
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