There was a sinister turban of black clouds wrapped around the summit
of the great peak, and before we were half-way up what had only been a
cold rain in the lower valley was turning into driving sleet and snow.
We ascended by the first _teleferica_--a double one--without
difficulty, but the ominous swaying of the cables warned us that the
next line, which was more exposed, might be quite another matter. This
latter is the one I have mentioned as running from an Alpine meadow to
the brow of a cliff towering three thousand feet above it. It was one
of the longest--if not the longest--unsupported cable-spans on the
whole Alpine front. It was also the steepest of which I had had any
experience. The fact that it was exposed throughout its whole length
to a strong wind which blew down from an upper valley was responsible
for putting it “out of business” during bad weather and thus made it
the weak link in the attenuated chain of the Adamello’s
communications.
As we had feared, we found this _teleferica_ “closed down” upon our
arrival at the lower station, ample reason for which appeared in the
fifteen or twenty-foot sway given to the parallel lines of cable by
the powerful “side-on” wind gusts which assailed it every few moments
from the direction of the glacier. Fortunately, as the storm was only
coming in fitful squalls as yet and had not settled down to a steady
blow, the _tenente_ in charge thought that it might be possible to
send us up in one of the quieter intervals.
“There’s no danger of the baskets blowing off the cable,” he said;
“it’s only a matter of preventing them striking one another in
passing, of which there is always risk when the wires are swaying too
much.”
Public-domain text, read in full here on John Shaqi.
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