Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.
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At The Moment When He Fell, He Plunged A Dagger Into The
Bosom Of His Only Daughter, "That She Might
Not have to blush before
the Spaniards at the name of the daughter of a traitor." The soul of
the
Tyrant (such is the belief of the natives) wanders in the
savannahs, like a flame that flies the approach of men.* (* See volume
1 chapter 1.4.)
The second historical event connected with the name of Valencia is the
great incursion made by the Caribs of the Orinoco in 1578 and 1580.
That cannibal horde went up the banks of the Guarico, crossing the
plains or llanos. They were happily repulsed by the valour of Garcia
Gonzales, one of the captains whose names are still most revered in
those provinces. It is gratifying to recollect, that the descendants
of those very Caribs now live in the missions as peaceable husbandmen,
and that no savage nation of Guiana dares to cross the plains which
separate the region of the forests from that of cultivated land. The
Cordillera of the coast is intersected by several ravines, very
uniformly directed from south-east to north-west. This phenomenon is
general from the Quebrada of Tocume, between Petares and Caracas, as
far as Porto Cabello. It would seem as if the impulsion had everywhere
come from the south-east; and this fact is the more striking, as the
strata of gneiss and mica-slate in the Cordillera of the coast are
generally directed from the south-west to the north-east. Most of
these ravines penetrate into the mountains at their southern
declivity, without crossing them entirely. But there is an opening
(abra) on the meridian of Nueva Valencia, which leads towards the
coast, and by which a cooling sea-breeze penetrates every evening into
the valleys of Aragua. This breeze rises regularly two or three hours
after sunset.
By this abra, the farm of Barbula, and an eastern branch of the
ravine, a new road is being constructed from Valencia to Porto
Cabello. It will be so short, that it will require only four hours to
reach the port; and the traveller will be able to go and return in the
same day from the coast to the valleys of Aragua. In order to examine
this road, we set out on the 26th of February in the evening for the
farm of Barbula.
On the morning of the 27th we visited the hot springs of La Trinchera,
three leagues from Valencia. The ravine is very large, and the descent
almost continual from the banks of the lake to the sea-coast. La
Trinchera takes its name from some fortifications of earth, thrown up
in 1677 by the French buccaneers, who sacked the town of Valencia. The
hot springs (and this is a remarkable geological fact,) do not issue
on the south side of the mountains, like those of Mariara, Onoto, and
the Brigantine; but they issue from the chain itself almost at its
northern declivity. They are much more abundant than any we had till
then seen, forming a rivulet which, in times of the greatest drought,
is two feet deep and eighteen wide. The temperature of the water,
measured with great care, was 90.3 degrees of the centigrade
thermometer. Next to the springs of Urijino, in Japan, which are
asserted to be pure water at 100 degrees of temperature, the waters of
the Trinchera of Porto Cabello appear to be the hottest in the world.
We breakfasted near the spring; eggs plunged into the water were
boiled in less than four minutes. These waters, strongly charged with
sulphuretted hydrogen, gush out from the back of a hill rising one
hundred and fifty feet above the bottom of the ravine, and tending
from south-south-east to north-north-west. The rock from which the
springs gush, is a real coarse-grained granite, resembling that of the
Rincon del Diablo, in the mountains of Mariara. Wherever the waters
evaporate in the air, they form sediments and incrustations of
carbonate of lime; possibly they traverse strata of primitive
limestone, so common in the mica-slate and gneiss of the coasts of
Caracas. We were surprised at the luxuriant vegetation that surrounds
the basin; mimosas with slender pinnate leaves, clusias, and
fig-trees, have pushed their roots into the bottom of a pool, the
temperature of which is 85 degrees; and the branches of these trees
extended over the surface of the water, at two or three inches
distance. The foliage of the mimosas, though constantly enveloped in
the hot vapours, displayed the most beautiful verdure. An arum, with a
woody stem, and with large sagittate leaves, rose in the very middle
of a pool the temperature of which was 70 degrees. Plants of the same
species vegetate in other parts of those mountains at the brink of
torrents, the temperature of which is not 18 degrees. What is still
more singular, forty feet distant from the point whence the springs
gush out at a temperature of 90 degrees, other springs are found
perfectly cold. They all follow for some time a parallel direction;
and the natives showed us that, by digging a hole between the two
rivulets, they could procure a bath of any given temperature they
pleased. It seems remarkable, that in the hottest as well as the
coldest climates, people display the same predilection for heat. On
the introduction of Christianity into Iceland, the inhabitants would
be baptized only in the hot springs of Hecla: and in the torrid zone,
in the plains, as well as on the Cordilleras, the natives flock from
all parts to the thermal waters. The sick, who come to La Trinchera to
use vapour-baths, form a sort of frame-work over the spring with
branches of trees and very slender reeds. They stretch themselves
naked on this frame, which appeared to me to possess little strength,
and to be dangerous of access. The Rio de Aguas Calientes runs towards
the north-east, and becomes, near the coast, a considerable river,
swarming with great crocodiles, and contributing, by its inundations,
to the insalubrity of the shore.
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