Gleanings in Europe : $b Italy, vol. 1 of 2Cooper, James Fenimore
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Gleanings in Europe : $b Italy, vol. 1 of 2
Cooper, James Fenimore
Cooper, James Fenimore, 1789-1851 -- Travel -- Italy; Italy -- Description and travel
The ascent is rather steeper than the sides of a pile of gravel would
be, supposing it to have been formed by the falling of the material on
a given place, without a force sufficient to change its outline. It
appeared to me to be at an angle of about fifty or fifty-five degrees
with the plane of the horizon. As the cinders yield with the weight
of a man, the foot sinking often to the instep, it is a severe task
to get up this place. We went at it coolly, but steadily, stopping to
take breath after short efforts; and I believe we were about twenty
minutes in reaching the summit. The cinders were warm in spots, and a
sulphurous smoke issued from the cone in a great many places that we
passed. I was too experienced a traveller to run myself out of breath,
as the moment of enjoyment approached. Having got within a few feet
of the top, I paused to recover breath; poor W----, who had commenced
with fury, being still a hundred feet beneath me. The guide waited my
leisure; but the guard, whose duty compelled him to go no further than
the foot of the cone, but who, being on his first excursion, chose to
ascend also, lay panting on the rim of the cone, or crater, as I put my
foot by his side.
This was another novel and beautiful _coup d’œil_. As the place was
very different from what I had expected to see, I shall endeavour to
make you understand what it really is. It appeared to me that the
depth of the great crater, at the place where we stood, was a little
more than half of the descent of the cone itself, on its exterior:
though its edge is ragged, and at one spot was two or three hundred
feet higher than at that which we had reached. This edge of the cone,
or crater, overhung its sides in nearly the whole circuit, and the
distance round it was near or quite a mile. It follows, that the
diameter of the crater must be about a third of a mile. Its bottom was
like a floor of clay, resembling that of the Solfatara, smoke issuing
from its crevices. Vivid streaks of brimstone gave it wild, unnatural
tints. It seemed quite as level as an ordinary brick-yard, viewed
from our stand. A little on one side of this circular plain, rose a
small cone, which might be a hundred and fifty or two hundred feet
high, formed of the same materials as the outer cone, with an orifice
perhaps some eighty or a hundred feet in width. This was the living, or
true crater. Out of this spot issued all the smoke, fire, stones, and
cinders of the ordinary workings of the mountain, of which, in truth,
it is the safety valve. This little haystack-looking cone was nearer
to the eastern and southern edges of the great crater than to the
northern and western, and it is altogether too low to be visible to any
except those who ascend to the place we occupied. The red-hot stones
must therefore be propelled upwards many hundred feet, perhaps six or
eight, to be seen at Naples or Sorrento, where we have often seen them,
however, of late.
Public-domain text, read in full here on John Shaqi.
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