Wintering in the Riviera: With Notes of Travel in Italy and France, and Practical Hints to Travellers
John Stuart Mill · en
We were anxious upon our return to Naples to have ascended Vesuvius,
at least as far as the Observatory, but unfortunately a heavy cloud
hung over the mountain, and reluctantly we had to give it up. Instead,
we took a drive to Puteoli, or, as it is now called, Pozzuoli, about
two hours distant. Our way lay through the grotto of Posilipo, which
is lighted up with gas, and is about a third of a mile long, about 21
feet wide, and varies in height from 70 to 25 feet; thence along an
uninteresting road till again we reached the sea, when the islands
and Puteoli looked very picturesque. One could hardly imagine from
its appearance that it was formerly a great Roman port; but it has
been subjected to many changes, and bears evidence of the forces
below agitating the ground, by which some parts have been alternately
submerged and upheaved, and the recurrence of such events would be
sufficient of themselves to account for its desertion. Here we drove
over the southern termination of the Appian Way, paved with the large
old Roman stones; and our coachman pointed out the part of the old
Roman pier (now in fragments, like a row of giant stepping–stones
lifting their heads above water) at which he alleged the Apostle
Paul had landed. There are some ruined temples in Puteoli and its
neighbourhood, and the ruins of a large amphitheatre, which the guide
said had held 45,000, but, as is more credibly stated by others, 25,000
spectators, for it is not so large or so imposing as that at Nismes,
while the measurements are considerably less,—Nismes exceeding it in
length by 75 feet, and in breadth by 120 feet. Chambers underneath were
discovered in 1838, and are very interesting. They contained dens for
the confinement of the wild beasts, and rooms where the gladiators were
trained to fight. We had, previous to entering Puteoli, taken a side
road to Solfatara. This is a scarcely extinct crater, supposed to have
a direct communication underground with Vesuvius, twelve miles distant.
However, there has been no eruption since 1198, when it sent forth a
current of lava. A man who appeared as guide threw a heavy stone upon
the probably thin crust of sulphurous matter constituting the ground
over which we were treading; the reverberation from the fall indicated
that it was hollow below, and in all likelihood a slender protection
from a fiery furnace which it might not be safe to expose to the air
and light of day. And as Solfatara is quiescent when Vesuvius is
active, and active when Vesuvius is quiescent, which it then was, the
thought, as we were intruding upon the domains of these angry forces of
nature, that some sudden impulse might burst the earthy covering and
blow us all up into the air, like Paul Pry peering about the steamboat
when the boiler burst, was not comfortable. The guide took us to a hole
from which sulphurous fumes were issuing, and for a few coppers entered
it at some risk of suffocation, and by means of a long stick pulled