_The swing of mountains._—If an earthquake wave is passing through
ground the surface of which is level, so long as this ground is
homogeneous, as the wave travels further and further we should expect
its energy to become less and less, until, finally, it would insensibly
die out. If, however, we have standing upon this plain a mountain,
judging from Mallet’s remarks, this mountain would be set in a state
of vibration much in the same way as a house is set in vibration,
and it would tend to oscillate backward and forward with a period of
vibration dependent upon the nature of its materials, size, and form.
The upper portion of this mountain would, in consequence, swing through
a greater arc than the lower portion, and buildings situated on the top
of it would swing to and fro through a greater arc than those which
were situated near its foot. This explanation why buildings situated
on the top of a mountain should suffer more than those situated on
a plain, is one which was offered by Mallet when writing of the
Neapolitan earthquake. He tells us that towns on hills are ‘rocked as
on the top of masts,’ and if we accept this explanation it would, in
fact, be one reason why the houses situated on the Bluff at Yokohama
suffered more than those situated in the settlement. This explanation
is given on account of the great authority it claims as a consequence
of its source. It is not clear how the statement can be supported,
as different portions of the mountain receive momentum in opposite
directions at the same time.
Public-domain text, read in full here on John Shaqi.
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