Observations on Mount Vesuvius, Mount Etna, and Other Volcanos — John Shaqi
Observations on Mount Vesuvius, Mount Etna, and Other VolcanosHamilton, William, Sir
Science
Observations on Mount Vesuvius, Mount Etna, and Other Volcanos
Hamilton, William, Sir
Etna, Mount (Italy) -- Early works to 1800; Vesuvius (Italy) -- Early works to 1800; Volcanoes -- Italy -- Early works to 1800
certainly is a much greater variety in the erupted matter and lavas of
the latter, than of the former; both abound with pyrites and
crystallizations, or rather vitrifications. The sea shore at the foot of
Etna, indeed, abounds with amber, of which there is none found at the
foot of Vesuvius. At present there is a much greater quantity of sulphur
and salts on the top of Vesuvius than on that of Etna; but this
circumstance varies according to the degree of fermentation within; and
our guide assured me, he had seen greater quantities on Etna at other
times. In our way back to Catania, the Canon shewed me a little hill,
covered with vines, which belonged to the Jesuits, and, as is well
attested, was undermined by the lava in the year 1669, and transported
half a mile from the place where it stood, without having damaged the
vines.
In great eruptions of Etna, the same sort of lightning, as described in
my account of the last eruption of Vesuvius, has been frequently seen to
issue from the smoak of its great crater. The antients took notice of
the same phaenomenon; for Seneca (lib. ii. Nat. Quaest.) says,--"AEtna
aliquando multo igne abundavit, ingentem vim arenae urentis effudit,
involutus est dies pulvere, populosque subita nox terruit, _illo tempore
aiunt plurima fuisse tonitrua et fulmina_."
Till the year 252 of Christ, the chronological accounts of the eruptions
of Etna are very imperfect: but as the veil of St. Agatha was in that
year first opposed to check the violence of the torrents of lava, and
has ever since been produced at the time of great eruptions; the
miracles attributed to its influence, having been carefully recorded by
the priests, have at least preserved the dates of such eruptions. The
relicks of St. Januarius have rendered the same service to the lovers of
natural history, by recording the great eruptions of Vesuvius. I find,
by the dates of the eruptions of Etna, that it is as irregular and
uncertain in its operations as Vesuvius[25]. The last eruption was in
1766.
On our return from Messina to Naples, we were becalmed three days in the
midst of the Lipari islands, by which we had an opportunity of seeing
that they have all been evidently formed by explosion[26]; one of them,
called Vulcano, is in the same state as the Solfaterra. Stromboli is a
Volcano, existing in all its force, and, in its form of course, is the
most pyramidal of all the Lipari Islands; we saw it throw up red hot
stones from its crater frequently, and some small streams of lava issued
from its side, and ran into the sea[27]. This Volcano differs from Etna
and Vesuvius, by its continually emitting fire, and seldom any lava;
notwithstanding its continual explosions, this island is inhabited, on
one side, by about an hundred families.
[Illustration: _Plate V._
STROMBOLI, one of the LIPARI ISLANDS.]
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