be) accomplished.[138] On the Italian half, the rock is throughout,
schist, and the gradient, being only one in 2,000, or 2-8/25 per mile,
all the elements for progress will continue to be, comparatively, as
favourable as they have hitherto been; and even with a much less rapid
rate of advance than on the French side, it requires no great gift of
prophesy to “forecaste” that the boring machines from Italy will be
ready to embrace those from France long before the latter shall have
arrived at the midway point. But let it be understood that the works
from the Italian side cannot go on a yard beyond midway,—first, on
account of the gradient, which would dam up all the water percolating
into the tunnel; second, because it would be impossible to keep the
line of the tunnel, owing to the absence of all the external landmarks
required for ensuring its correct direction. The embrace we have just
referred to will take place 4,138 feet above the level of the sea,
1,645 above the level of St. Michel, 429 above the Modane entrance of
the tunnel, but only 2-8/25 above that at Bardoneche, 2,360 above the
level of Susa, about 5,360 feet _below_ the highest point of the Great
Vallon Mountain, and 2,520 feet below the summit of the Mont Cenis
Railway.
What might have proved a source of great trouble and expense—water—has
fortunately not as yet on any one occasion presented itself in a manner
to cause alarm or even uneasiness. We need not therefore refer to
this subject in any detail, but before proceeding to as important an
element as any with which the tunnel is encompassed—cost—we had better
state that the arch of the tunnel is a semicircle 25 feet 3½ inches at
its base, 26 feet 3 at its broadest part, and 24 feet 7 inches high.
(See diagram.)
Public-domain text, read in full here on John Shaqi.
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