The movement of tectonic plates causes earthquakes, such as the Great Alaska Earthquake of 1964. Major earthquakes provide critical information about Earth's interior and highlight the importance of preparedness. Examples include the 2011 earthquake in Japan and historic seismic events along the San Andreas Fault in California and the Great Kanto Earthquake in Tokyo.
Earthquakes demonstrate the dynamic nature of our planet, often caused by the movement of tectonic plates. An example of this is the Great Alaska Earthquake of 1964, which was the most powerful quake to strike the United States.
This and other earthquakes provide valuable insights into Earth's interior and the forces that shape our world.
Japan's 2011 earthquake off the coast of Honshu, which led to over 15,500 deaths, was another significant seismic event, also causing a devastating tsunami.
The regularity of seismic activity at plate boundaries acts as reminders of the inherent geological risks associated with living near these zones, such as those experienced in California with the San Andreas Fault and historically, in the 1923 Great Kanto Earthquake in Japan.
Studying these events helps us understand the Earth's geology and the importance of preparedness and resilient infrastructure to minimize the impact of such natural disasters.