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Updated: May 23, 2025
It was a circumstance I was interested in, having first met with the camel at Teneriffe and the Cape Verd Islands, the westernmost limit of its distribution; imported thither, however, as it now is into Australia, where, though there is no Acacia Arabica, four hundred other species of the genus are known.
Furthermore the conquest of the Canaries at the end of the fourteenth century and of Teneriffe and other islands in the fifteenth led to the bringing of many of their natives as slaves to Castille and the neighboring kingdoms.
The peak of Teneriffe, for instance, lies in the sub-tropical zone, but, at the elevation named, we meet with the vegetation which characterizes the warm temperate zone. And this holds true of all our mountain systems, in all latitudes, and at all altitudes, in all parts of the globe.
Von Buch has described a stream of obsidian on the Peak of Teneriffe, in which the crystals of feldspar become more and more numerous, as the depth or thickness increases, so that near the lower surface of the stream the lava even resembles a primary rock. In these cases, I presume there can be no doubt that the crystals sink from their weight.
The Peak of Teneriffe, Mount Etna, and several others, also rise above the snow-line; while the burning mountains of Iceland, Greenland, and Kamtschatka, with those which rear their heads in the frozen regions near the South Pole, are for the most part enveloped in ice and snow from head to foot.
I had in my hand, on board the Pizarro, a journal, in which it was noted, that the peak of Teneriffe had been seen at 135 miles distance, near the southern cape of Lancerota, called Pichiguera. Its summit was discovered under an angle considerable enough to lead the observer, Don Manual Baruti, to conclude that the volcano might have been visible at nine miles farther.
But this is anticipating. It was on the 23rd of December, 1894, that we left Liverpool in the Batanga, commanded by my old friend Captain Murray, under whose care I had made my first voyage. On the 30th we sighted the Peak of Teneriffe early in the afternoon. It displayed itself, as usual, as an entirely celestial phenomenon. A great many people miss seeing it.
On the 6th of January we reached Teneriffe, but were prevented landing, by fears of our bringing the cholera: the next morning we saw the sun rise behind the rugged outline of the Grand Canary Island, and suddenly illumine the Peak of Teneriffe, whilst the lower parts were veiled in fleecy clouds. This was the first of many delightful days never to be forgotten.
On September 8 a definite start was made, and when the lovely Canary Islands and the Peak of Teneriffe sank beneath the horizon, the sailors wept, believing that wind and sails would carry them from the world for ever, and that nothing but water and waves awaited them in the west.
The Cape de Verde Islands, which contain beds of limestone along with volcanic matter, possess in the island of Fuego an active volcano, rising to a height of 7000 feet above the surface of the ocean. The central cone, like that of Teneriffe, rises from within an outer crater, formed of basalt alternating with beds of agglomerate, and traversed by numerous dykes of lava.
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