What Causes Earthquakes Around The World

what causes earthquakesEarthquakes can be caused by many events. So what causes earthquakes around the world? The most common causes of earthquakes are tectonic plates shifting and volcanic eruptions. However, the tectonic plates earthquakes happen more often than the volcanic eruption one. There are many countries which are at risk of getting earthquakes. Those countries are mostly in Asia such as Japan and Indonesia. However, places like North America, Peru, and other American countries can also be attacked by earthquakes. Thus, it is very important to prepare the resident for any unexpected earthquake. Modern countries like Japan and the United States of America are actively trained their resident to find safe shelters in case of earthquakes and other disasters phenomenon.

What Causes Earthquakes In Asia

People often ask about what causes earthquakes in Asia. Earthquakes in Asia are commonly caused by the shifting of tectonic plates and volcanic eruptions. Earthquakes can also happen because some of the earth upper mantles move past each other. This can cause tremendous energy and lead to powerful earthquakes. If the earthquake happens below the sea, it can cause another disastrous phenomenon that is usually called a tsunami. A tsunami can be deadly for those who are living on the beach. Therefore, it is best for the people on the beach to evacuate after an earthquake happens. It is highly recommended for the government to actively train their residents for a disaster such as earthquakes and tsunami.

A tsunami can be predicted by modern technology and scientist can warn the people of the disaster. However, the predictions are sometimes not accurate. Therefore, you cannot be too careful about tsunami and earthquakes. Countries with multiple active volcanos are also in danger of earthquake attacks. Asian countries such as Indonesia can be at risk of tectonic plates and volcanic earthquakes. Hopefully, this article can answer your question about what causes earthquakes.

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