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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According To The
Statements Of The Ancients, The Mons Albanus, Near Rome, Known At
Present Under The Name Of Monte
Cavo, appeared at times on fire
during the night; but the Mons Albanus is a volcano recently
extinguished, which, in
The time of Cato, threw out rapilli;* (*
"Albano monte biduum continenter lapidibus pluit." - Livy lib. 25
cap. 7. (Heyne, Opuscula Acad. tome 3 page 261.)) while the
Cuchivano is a calcareous mountain, remote from any trap formation.
Can these flames be attributed to the decomposition of water,
entering into contact with the pyrites dispersed through the
schistose marl? or is it inflamed hydrogen that issues from the
cavern of Cuchivano? The marls, as the smell indicates, are
pyritous and bituminous at the same time; and the petroleum springs
at the Buen Pastor, and in the island of Trinidad, proceed probably
from these same beds of alpine limestone. It would be easy to
suppose some connexion between the waters filtering through this
calcareous stone, and decomposed by pyrites and the earthquakes of
Cumana, the springs of sulphuretted hydrogen in New Barcelona, the
beds of native sulphur at Carupano, and the emanations of
sulphurous acid which are perceived at times in the savannahs. It
cannot be doubted also, that the decomposition of water by the
pyrites at an elevated temperature, favoured by the affinity of
oxidated iron for earthy substances, may have caused that
disengagement of hydrogen gas, to the action of which several
modern geologists have attributed so much importance. But in
general, sulphurous acid is perceived more commonly than hydrogen
in the eruption of volcanoes, and the odour of that acid
principally prevails while the earth is agitated by violent shocks.
When we take a general view of the phenomena of volcanoes and
earthquakes, when we recollect the enormous distance at which the
commotion is propagated below the basin of the sea, we readily
discard explanations founded on small strata of pyrites and
bituminous marls.
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