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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The Captain Of The Brig
Denied The Fact; And Asserted That, Far From Having Introduced The
Malady, His Crew Had Caught It In The Port.
We know from what
happened at Cadiz in 1800, how difficult it is to elucidate facts,
when their uncertainty serves to favour theories diametrically
opposite one to another.
The more enlightened inhabitants of
Caracas and La Guayra, divided in opinion, like the physicians of
Europe and the United States, on the question of the contagion of
yellow fever, cited the instance of the American vessel; some for
the purpose of proving that the typhus had come from abroad, and
others, to show that it had taken birth in the country itself.
Those who advocated the latter opinion, admitted that an
extraordinary alteration had been caused in the constitution of the
atmosphere by the overflowings of the Rio de La Guayra. This
torrent, which in general is not ten inches deep, was swelled after
sixty hours' rain in the mountains, in so extraordinary a manner,
that it bore down trunks of trees and masses of rock of
considerable size. During this flood the waters were from thirty to
forty feet in breadth, and from eight to ten feet deep. It was
supposed that, issuing from some subterranean basin, formed by
successive infiltrations, they had flowed into the recently cleared
arable lands. Many houses were carried away by the torrent; and the
inundation became the more dangerous for the stores, in consequence
of the gate of the town, which could alone afford an outlet to the
waters, being accidentally closed. It was necessary to make a
breach in the wall on the sea-side. More than thirty persons
perished, and the damage was computed at half a million of
piastres. The stagnant water, which infected the stores, the
cellars, and the dungeons of the public prison, no doubt diffused
miasms in the air, which, as a predisposing cause, may have
accelerated the development of the yellow fever; but I believe that
the inundation of the Rio de la Guayra was no more the primary
cause, than the overflowings of the Guadalquivir, the Xenil, and
the Gual-Medina, were at Seville, at Ecija, and at Malaga, the
primary causes of the fatal epidemics of 1800 and 1804. I examined
with attention the bed of the torrent of La Guayra; and found it to
consist merely of a barren soil, blocks of mica-slate, and gneiss,
containing pyrites detached from the Sierra de Avila, but nothing
that could have had any effect in deteriorating the purity of the
air.
Since the years 1797 and 1798, at which periods there prevailed
dreadful mortality at Philadelphia, St. Lucia, and St. Domingo, the
yellow fever has continued its ravages at La Guayra. It has proved
fatal not only to the troops newly arrived from Spain, but also to
those levied in parts remote from the coasts, in the llanos between
Calabozo and Uritucu, regions almost as hot as La Guayra, but
favourable to health.
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