After a week's halt at Naples, Sir Charles resumed his journey to
Sicily, landing at Messina on September 10th. By the 15th he was once
more on the slopes of Etna, and had begun a twelve-day period of hard
work on the mountain, passing five nights in very rough quarters at the
Casa degli Inglesi, 9,600 feet above sea-level. During this stay he
ascended the principal cone, carefully examining both the larger and the
smaller craters, and descended into the Val del Bove, a laborious
expedition, but one which well repaid him by throwing much light on the
structure of the volcanic mass. Still he was not yet satisfied, for
after he had descended to Zafarana, he returned to spend another night
at the Casa degli Inglesi in order to satisfy himself about one or two
details. From Zafarana also he went again to the Val del Bove, checking
and increasing his notes, and devoted another day to a most interesting
excursion through picturesque scenery as far as the watershed between
this vast hollow in the mountain side and the neighbouring Val di
Tripodo. On all these excursions Sir Charles, as far as possible, rode,
remarking to his wife, "I feel here that a good mule is like presenting
an old geologist with a young pair of legs." Work on the mountain ended,
he spent a little time in examining the Tertiary beds of the
neighbouring lowland, and then, getting back to Messina about the middle
of October, returned in due course to England.
These two journeys in succession greatly augmented his knowledge of the
structure of volcanic cones, and enabled him to deal the death-blow to
the "crater of elevation" hypothesis which had found such favour among
Continental geologists. He could now prove that lava would solidify in a
compact form on slopes of thirty-five or even forty degrees--a fact
which had been stoutly denied by advocates of that hypothesis, and was
able to offer an explanation of the singular structure of the Val del
Bove, viz. that it was a huge gulf, formed by a series of mighty
explosions, similar to those which shattered half of the old crater of
Vesuvius,[130] and sent one side of Bandai San[131] flying through the
air. He returned to England satisfied that his feet were on firm ground,
if such a phrase be permissible in regard to a volcano, and that the
results[132] of this conscientious labour in the fulness of his age had
strengthened him in the position which he had adopted in his scientific
youth.
Public-domain text, read in full here on John Shaqi.
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