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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I Do Not Pretend To Form
Any Opinion In Favour Of The Existence Of The Atlantis; But I
Endeavour To
Prove, that the Canaries have no more been created by
volcanoes, than the whole body of the smaller Antilles has
Been
formed by madrepores.) is by no means contradictory to the
acknowledged laws of nature; and that nothing opposes the
supposition that the summits of Porto Santo, Madeira, and the
Fortunate Islands, may heretofore have formed, either a distinct
range of primitive mountains, or the western extremity of the chain
of the Atlas.
The peak of Teyde forms a pyramidal mass like Etna, Tungurahua, and
Popocatepetl. This physiognomic character is very far from being
common to all volcanoes. We have seen some in the southern
hemisphere, which, instead of having the form of a cone or a bell,
are lengthened in one direction, having the ridge sometimes smooth,
and at others bristled with small pointed rocks. This structure is
peculiar to Antisana and Pichincha, two burning mountains of the
province of Quito; and the absence of the conic form ought never to
be considered as a reason excluding the idea of a volcanic origin.
I shall develop, in the progress of this work, some of the
analogies, which I think I have perceived between the physiognomy
of volcanoes and the antiquity of their rocks. It is sufficient to
state, generally speaking, that the summits, which are still
subject to eruptions of the greatest violence, and at the nearest
periods to each other, are SLENDER PEAKS of a conic form; that the
mountains with LENGTHENED SUMMITS, and rugged with small stony
masses, are very old volcanoes, and near being extinguished; and
that rounded tops, in the form of domes, or bells, indicate those
problematic porphyries, which are supposed to have been heated in
their primitive position, penetrated by vapours, and forced up in a
mollified state, without having ever flowed as real lithoidal
lavas.
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