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The term earthquake is applied to any tremor or shaking of the ground Many earthquakes are se gentle as to pour aims
unrecognised other are sufficiently pronounced to exette general alarm while some spread enormous destruction Desvete
earthquakes are usually confined to Amited regions. The usual phenomena recorded in well-known earthquaketare
Wembling next one or more severe shocks, and then a trembling which gradually dles away. In most cases each shoclo
only a lew seconds, but the tremblings that follow may continue for days, weeks or even months Noises of various kinds
accompany an earthquake. They have been ikened to the howling of storm, the growing of thunder the clanking and closing
ofron e hains of the rumbling of heavy wagons along a rood Such noisex ore conducted through the ground or they may
travel tough the sea oral and are often heard of great distances trom the place where the shock is felt some earthquakes
however, are not accompanied by there nolsex At the time of the terrible shock which destroyed Riobamba in Ecuador on
February 1797. o complete allence reloned.
Meny changes are produced on the north's surface by earthquakes. They cause landslips and cracks in the earth, which
rometimes after the drainage system of a country. They are trequently accompanied by great sea woves, which will often
sweep rocks and sand great distances inland. Permanent elevations and depressions of land are sometimes couled Anthe
great earthquakes of 1750, the cool of Chili wos lound to have been permanently raised from three to four feet well-known
exemples of permanent depressions are those of the Runn of Kutch and the coasttands near Chittagong, which suddenly sank
during the Bengol earthquake of 1742
Earthquakes are the most common in volcanic and mountainous regions and many of them are no doubt due to volcanic
aetion. These appear to originate in the sea, and may be due to the flashing into steam of the water which finds its way down
through crocks to the underlying heated rocks Others oppear to originate in volcanoes themselves, being due to the explosion
of vapours which expond Many other causes ore aseribed, of which two may be mentioned. Some earthquakes may be due to
the collapse of hollows beneath the ground, and others again to the snapping of stato which has been subjected to toe te
strain is noticeable that most earthquakes occur during the cold months of winter.
Among destructive earthquakes in modern times may be mentioned the one that offered the half of Messina bawy
and sichy in 1908 and the terrible upheaval in Japan in 1925, which destroyed whole towns and caused the death of thousands
of people​

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Answered by ala036628
1

Answer:

yes

Explanation:

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