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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Colonel Franqui Assured Borda, That
The Place Is Still To Be Seen Whence The Melted Matter Issued; And
That The Ashes Which Covered The Ground Adjacent, Were Not Yet
Fertilized.
Whenever the rock appeared, we discovered basaltic
amygdaloid* (* Basaltartiger Mandelstein.
Werner.) covered with
hardened clay,* (* Bimstein-Conglomerat. W.) which contains
rapilli, or fragments of pumice-stone. This last formation
resembles the tufas of Pausilippo, and the strata of puzzolana,
which I found in the valley of Quito, at the foot of the volcano of
Pichincha. The amygdaloid has very long pores, like the superior
strata of the lavas of Vesuvius, arising probably from the action
of an elastic fluid forcing its way through the matter in fusion.
Notwithstanding these analogies, I must here repeat, that in all
the low region of the peak of Teneriffe, on the side of Orotava, I
have met with no flow of lava, nor any current, the limits of which
are strongly marked. Torrents and inundations change the surface of
the globe, and when a great number of currents of lava meet and
spread over a plain, as I have seen at Vesuvius, in the Atrio dei
Cavalli, they seem to be confounded together, and wear the
appearance of real strata.
The villa de Orotava has a pleasant aspect at a distance, from the
great abundance of water which runs through the principal streets.
The spring of Agua Mansa, collected in two large reservoirs, turns
several mills, and is afterward discharged among the vineyards of
the adjacent hills. The climate is still more refreshing at the
villa than at the port of La Cruz, from the influence of the
breeze, which blows strong after ten in the morning. The water,
which has been dissolved in the air at a higher temperature,
frequently precipitates itself; and renders the climate very foggy.
The villa is nearly 160 toises (312 metres) above the level of the
sea, consequently 200 toises lower than the site on which Laguna is
built: it is observed also, that the same kind of plants flower a
month later in this latter place.
Orotava, the ancient Taoro of the Guanches, is situated on a very
steep declivity. The streets seem deserted; the houses are solidly
built, and of a gloomy appearance. We passed along a lofty
aqueduct, lined with a great number of fine ferns; and visited
several gardens, in which the fruit trees of the north of Europe
are mingled with orange trees, pomegranate, and date trees. We were
assured, that these last were as little productive here as on the
coast of Cumana. Although we had been made acquainted, from the
narratives of many travellers, with the dragon-tree of the garden
of M. Franqui, we were not the less struck with its enormous
magnitude. We were told, that the trunk of this tree, which is
mentioned in several very ancient documents as marking the
boundaries of a field, was as gigantic in the fifteenth century as
it is at the present time.
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