EARTHQUAKES
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foundations had been weakened by drainage when the
water was withdrawn from its front during the advance of
the earthquake wave, and it slid down the mud slope into
the river. The Lisbon Earthquake was recorded in France
only in the extreme S.W.; but it has been assigned an un-
usually wide range as a shock in Derbyshire has been attri-
buted to it, but was doubtless due to an independent local
sarthquake.
Along earthquake stricken coasts most of the destruction
is often wrought by a huge wave which rolls in from the sea.
Harbours and coast towns in seismic belts are only safe if
sheltered from the open sea, or above the reach of earthquake
waves.
Some strongly constructed buildings collapsed during the
San Francisco Earthquake in 1906, as they were erected on
land made by filling bays with loose material, and the weak
foundations had given trouble before the earthquake.
Similar buildings on firm ground were only shaken, though
some were destroyed by fire.
The most fatal earthquake for which there are accurate
records was at Tokyo on the 1st September, 1923; the official
roll of killed and missing is 142,807. The shock there was
moderate; well-built masonry buildings and even fragile
structures on their roofs were not injured. The loss of life
was due to the earthquake happening just before the midday
meal; the charcoal braziers used for cooking were over-
thrown ; fallen laths and scraps of wallpaper were ignited ;
and many fires broke out simultaneously. The people
flocked for shelter into open spaces where they were suffo-
cated by smoke. The damage at Tokyo was estimated at
£1,000,000,000, of which 95 per cent. was due to fire.
B. Anti-EarTHQUARE ConsTRUCTION—No ordinary build-
ing can resist the most violent grade of earthquake without
serious damage. In the Assam Earthquake of 1896 Shillong
was jerked 18 inches to and fro 200 times a minute. Walls
were shaken to pieces and the roofs settled down over piles
of broken masonry. Tree trunks were snapped across just
above the ground. This terrific oscillation was combined
with an upward jerk by which huge stones were hurled into
the air, at an angle of over 60°; after rising 4 feet they
struck the ground 6% feet from their original position,