Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.
- Page 184 of 208 - First - Home
At
This Spot The Valley Of Caracas Communicates, By The Valleys Of
Tacagua And Of Tipe, With The Coast Near Catia.
A ridge of rock,
the summit of which is forty toises above the bottom of the valley
of Caracas, and more than three hundred toises above the valley of
Tacagua, divides the waters which flow into the Rio Guayra and
towards Cabo Blanco.
On this point of division, at the entrance of
the branch, the view is highly pleasing. The climate changes as we
descend westward. In the valley of Tacagua we found some new
habitations, and also conucos of maize and plantains. A very
extensive plantation of tuna, or cactus, stamps this barren country
with a peculiar character. The cactuses reach the height of fifteen
feet, and grow in the form of candelabra, like the euphorbia of
Africa. They are cultivated for the purpose of selling their
refreshing fruits in the market of Caracas. The variety which has
no thorns is called, strangely enough, in the colonies, tuna de
Espana (Spanish cactus). We measured, at the same place, magueys or
agaves, the long stems of which, laden with flowers, were
forty-four feet high. However common this plant is become in the
south of Europe, the native of a northern climate is never weary of
admiring the rapid development of a liliaceous plant, which
contains at once a sweet juice and astringent and caustic liquids,
employed to cauterize wounds.
We found several veins of quartz in the valley of Tipe visible
above the soil. They contained pyrites, carbonated iron-ore, traces
of sulphuretted silver (glasserz), and grey copper-ore (fahlerz).
The works which had been undertaken, either for extracting the ore,
or exploring the nature of its bed, appeared to be very
superficial. The earth falling in had filled up those excavations,
and we could not judge of the richness of the lode. Notwithstanding
the expense incurred under the intendancy of Don Jose Avalo, the
great question whether the province of Venezuela contains mines
rich enough to be worked, is yet problematical. Though in countries
where hands are wanting, the culture of the soil demands
unquestionably the first care of the government, yet the example of
New Spain sufficiently proves that mining is not always
unfavourable to the progress of agriculture. The best-cultivated
Mexican lands, those which remind the traveller of the most
beautiful districts of France and the south of Germany, extend from
Silao towards the Villa of Leon: they are in the neighbourhood of
the mines of Guanaxuato, which alone furnish a sixth part of all
the silver of the New World.
CHAPTER 1.14.
EARTHQUAKES AT CARACAS.
CONNECTION OF THOSE PHENOMENA WITH THE VOLCANIC ERUPTIONS
OF THE WEST INDIA ISLANDS.
On the evening of the 7th of February we took our departure from
Caracas. Since the period of our visit to that place, tremendous
earthquakes have changed the surface of the soil. The city, which I
have described, has disappeared; and on the same spot, on the
ground fissured in various directions, another city is now slowly
rising. The heaps of ruins, which were the grave of a numerous
population, are becoming anew the habitation of men. In retracing
changes of so general an interest, I shall be led to notice events
which took place long after my return to Europe. I shall pass over
in silence the popular commotions which have taken place, and the
modifications which society has undergone. Modern nations, careful
of their own remembrances, snatch from oblivion the history of
human revolutions, which is, in fact, the history of ardent
passions and inveterate hatred. It is not the same with respect to
the revolutions of the physical world. These are described with
least accuracy when they happen to be contemporary with civil
dissensions. Earthquakes and eruptions of volcanoes strike the
imagination by the evils which are their necessary consequence.
Tradition seizes on whatever is vague and marvellous; and amid
great public calamities, as in private misfortunes, man seems to
shun that light which leads us to discover the real causes of
events, and to understand the circumstances by which they are
attended.
I have recorded in this work all I have been able to collect, and
on the accuracy of which I can rely, respecting the earthquake of
the 26th of March, 1812. By that catastrophe the town of Caracas
was destroyed, and more than twenty thousand persons perished
throughout the extent of the province of Venezuela. The intercourse
which I have kept up with persons of all classes has enabled me to
compare the description given by many eye-witnesses, and to
interrogate them on objects that may throw light on physical
science in general. The traveller, as the historian of nature,
should verify the dates of great catastrophes, examine their
connection and their mutual relations, and should mark in the rapid
course of ages, in the continual progress of successive changes,
those fixed points with which other catastrophes may one day be
compared. All epochs are proximate to each other in the immensity
of time comprehended in the history of nature. Years which have
passed away seem but a few instants; and the physical descriptions
of a country, even when they offer subjects of no very powerful and
general interest, have at least the advantage of never becoming
old. Similar considerations, no doubt, led M. de la Condamine to
describe in his Voyage a l'Equateur, the memorable eruptions of the
volcano of Cotopaxi,* which took place long after his departure
from Quito. (* Those of the 30th of November, 1744, and of the 3rd
of September, 1750.) I feel the less hesitation in following the
example of that celebrated traveller, as the events I am about to
relate will help to elucidate the theory of volcanic reaction, or
the influence of a system of volcanoes on a vast space of
circumjacent territory.
At the time when M. Bonpland and myself visited the provinces of
New Andalusia, New Barcelona, and Caracas, it was generally
believed that the most eastern parts of those coasts were
especially exposed to the destructive effects of earthquakes.
Enter page number
PreviousNext
Page 184 of 208
Words from 186707 to 187728
of 211363