The land-area disturbed by the earthquake and the isoseismal lines are
shown in Fig. 25, the small black oval area (which Includes
Charleston) being that within which the greatest damage to buildings
occurred. The chief part of the epicentre, however, lies from 12 to 15
miles to the west and north-west of Charleston, in a forest-clad
district, containing only two villages and various scattered houses.
The city of Charleston, whose population between 1880 and 1891
increased from fifty to fifty-five thousand, is built on a peninsula
between the Cooper River on the east and the Ashley River on the
south-west. Originally, this was an irregular tract of comparatively
high and dry land, intersected by numerous creeks, which, as the city
grew, were filled up to the general level of the higher ground. It is
on this "made land" as a rule that the more serious damage to
buildings occurred.
At 9.51 P.M. (standard time of the 75th meridian), the great
earthquake occurred, and, one minute later, there was left hardly a
building in the city that was not injured more or less seriously. "The
destruction," as Major Dutton remarks, "was not of that sweeping and
unmitigated order which has befallen other cities, and in which every
structure built of material other than wood has been levelled
completely to the earth in a chaos of broken rubble, beams, tiles, and
planking, or left in a condition practically no better." The number of
houses entirely demolished was not great, but several hundred lost a
large part of their walls, and many were condemned as unsafe and
afterwards pulled down. A board of inspectors, appointed to
investigate the condition of the houses, reported that not one hundred
out of fourteen thousand chimneys examined by them escaped damage, and
that 95 per cent. of those injured were broken off at the roof. The
total cost of the necessary repairs, it was estimated, would amount to
about one million pounds.
According to the official records, 27 persons were killed in
Charleston during the earthquake, but, by cold, exposure, etc., this
number was brought up to not less than 83. The number of persons
wounded was never ascertained.
ISOSEISMAL LINES AND DISTURBED AREA.
Public-domain text, read in full here on John Shaqi.
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