Catalogue of Violent and Destructive Earthquakes in the Philippines: With an Appendix: Earthquakes in the Marianas Islands 1599-1909Saderra Masó, Miguel
History
Catalogue of Violent and Destructive Earthquakes in the Philippines: With an Appendix: Earthquakes in the Marianas Islands 1599-1909
Masonry arches were henceforth banished from the churches; the heavy
walls of the latter were further strengthened by massive buttresses;
and the towers were given truly enormous substructures. But even with
these precautions there is at present hardly one out of the hundreds
of churches built during the seventeenth and eighteenth centuries
which did not some time or other require important repairs of its
masonry work or even partial reconstruction owing to earthquake
damages. The only structure of this class which thus far has withstood
all convulsions, is the church of St. Agustin, Manila. Nevertheless,
as we have stated before, the chroniclers hardly mention all this
destruction, except in a very general and cursory manner. I do not
hesitate to say: they were accustomed to see similar havoc created
nearly every year in one part of the Archipelago or the other by some
severe typhoon, accompanied by far greater loss of lives and property,
and consequently much more felt by the people than the destruction of
a church, _convento_, municipal building ("tribunal"), one or two
bridges, or other masonry structure.
In the present catalogue our aim has been to present all that is known
of the various violent and destructive earthquakes on record. The
first column of each page contains the ordinal number of the
disturbance for purposes of reference. In the second, the date is
given as accurately as it could be ascertained, Roman numerals being
used to designate the months. Unfortunately, of some earthquakes only
the year is known; of others, the year and month. Of one (No. 32) the
approximate hour has been recorded, but not the day of the month;
while of another (No. 38) the hour has been preserved for posterity,
but whether the phenomenon occurred during February or March, the
records leave undecided. In the third column will be found, in the
first place, the intensity of the disturbance, Roman numerals
representing the degrees of the scale of De Rossi-Forel (I-X); then
the region affected most, and finally the damages caused, if known,
and other information, if available.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account