therefore, to invent instruments that neither slumbered nor slept. Some devices
were quite simple. one, for instance, consisted of rods of various lengths and
thicknesses which would stand up on end like ninepins. when a shock came it
shook the rigid table upon which these stood. If it were gentle, only the more
unstable rods fell. If it were severe, they all fell. Thus the rods by falling, and by
the direction in which they fell, recorded for the slumbering scientist the strength
of a shock that was too weak to waken him and the direction from which it came.
But instruments far more delicate than that were needed if any really serious
advance was to be made. The ideal to be aimed at was to devise an instrument
that could record with a pen on paper the movements, of the ground or of the
table, as the quake passed by. While I write my pen moves, but the paper keeps
still. With practice, no doubt, I could in time learn to write by holding the
still while the paper moved. That sounds a silly suggestion, but that was precisely
the idea adopted in some of the early instruments (seismometers) for recording
earthquake waves. But when table, penholder and paper are all moving how is
it possible to write legibly? The key to a solution of that problem lay in an every-
day observation. Why does a person standing in a bus or train tend to fall when
a sudden start is made? It is because his feet move on, but his head stays still.
A simple experiment will help us a little further. Tie a heavy weight at the end
of a long piece of string. With the hand held high in the air hold the strings so that
the weight nearly touches the ground. Now move the hand to and fro and around
but not up and down. It will be found that the weight moves but slightly or not
at all. Imagine a pen attached to the weight in such a way that its point rests upon
a piece of paper on the floor. Imagine an earthquake shock shaking the floor, the
paper, you and your hand. In the midst of all this movement the weight and the
pen would be still. But as the paper moved from side to side under the pen point
its movement would be recorded in ink upon its surface. It was upon this prin-
ciple that the first instruments were made, but the paper was wrapped round a
drum which rotated slowly. As long as all was still the pen drew a straight line,
but while the drum was being shaken the line that the pen was drawing wriggled
from side to side. The apparatus thus described, however, records only the
horizontal component of the wave movement, which is, in fact, much more com-
plicated. If we could actually see the path described by a particle, such as a sand
grain in the rock, it would be more like that of a bluebottle buzzing round the
room; it would be up and down, to and fro and from side to side. Instruments
have been devised and can he so placed that all three elements can be recorded
in different graphs.
When the instrument is situated at more than 700 miles from the earthquake
centre, the graphic record shows three waves arriving one after the other at
short intervals. The first records the arrival of longitudinal vibrations. The sec-
ond marks the arrival of transverse vibrations which travel more slowly and
arrive several minutes after the first. These two have travelled through the earth.
It was from the study of these that so much was learnt about the interior of the
earth. The third, or main wave, is the slowest and has travelled round the earth
through the surface rocks.
