Earthquakes and other earth movements — John Shaqi
Earthquakes and other earth movementsMilne, John
Science
Earthquakes and other earth movements
Milne, John
Earthquakes
The great advantage of continuously-moving machines is that the
beginning and end of the shock can usually be got with certainty, while
all the uncertainty as to the action of the ‘starter’ is avoided.
Self-starting machines have, of course, the advantage of simplicity and
cheapness, while there is no danger of the record getting obliterated
by the subsequent motion of the plate under the index.
_Time-recording Apparatus._—Of equal importance with the instruments
which record the motion of the ground, are those instruments which
record the time at which such motion took place. The great value of
time records, when determining the origin from which an earthquake
originates, will be shown farther on. The most important result which
is required in connection with time observations, is to determine
the interval of time taken by a disturbance in travelling from one
point to another. On account of the great velocity with which these
disturbances sometimes travel, it is necessary that these observations
should be made with considerable accuracy. The old methods of adapting
an apparatus to a clock which, when shaken, shall cause the clock to
stop, are of little value unless the stations at which the observations
are made are at considerable distances apart. This will be appreciated
when we remember that the disturbance may possibly travel at the rate
of a mile per second, that its duration at any station may often extend
over a minute, and that one set of apparatus at one station may stop,
perhaps, at the commencement of the disturbance, and the other near
the end. A satisfactory time-taking apparatus will therefore require,
not only the means for stopping a clock, but also a contrivance which,
at the same instant that the clock is stopped, shall make a mark on a
record which is being drawn by a seismograph. In this way we find out
at which portion of the shock the time was taken.
[Illustration: FIG. 7.]
Palmieri stops a clock in his seismograph by closing an electric
circuit. Mallet proposes to stop a clock by the falling of a column
which is attached by a string to the pendulum of the clock. So long as
the column is standing the string is loose and the pendulum is free
to move; but when the column falls, the string is tightened and the
pendulum is arrested. The difficulty which arises is to obtain a column
that will fall with a slight disturbance. The best form of contrivance
for causing a column to fall, and one which may also be used in drawing
out a catch to relieve the machinery of a record receiver, is shown in
the accompanying sketch.
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