Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.

































































































































 -  At
this spot the valley of Caracas communicates, by the valleys of
Tacagua and of Tipe, with the coast near - Page 184
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

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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.

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