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Dive into the intriguing world of earthquakes with us, uncovering the mysteries beneath our feet with simple explanations and engaging insights.
Our planet's surface is covered in large pieces called tectonic plates. Earthquakes often happen where these plates meet, moving against each other and causing the ground to shake.
Sometimes, smaller tremors called foreshocks happen before a big earthquake. These can hint at a larger quake on its way, giving scientists clues to predict future shakes.
After a major earthquake, smaller tremors called aftershocks frequently occur. These can add damage to structures already weakened by the main quake, posing additional risks.
Seismic waves are the energy that travels through the Earth during an earthquake, causing the ground to shake. The closer to the quake's center, the stronger the shaking.
The hypocentre is the deep underground starting point of an earthquake, where the shaking begins. Directly above the hypocentre is the epicentre, the surface point that experiences the strongest effects of the earthquake.
The most powerful earthquake recorded hit Chile on May 22, 1960. With a magnitude of 9.5, it shook the Earth for 10 minutes.
Japan experiences more earthquakes than any other country because it's located along the Pacific Ring of Fire, an area with a lot of tectonic activity.
Countries like the Philippines, the United States, and Chile also face many earthquakes due to their locations near tectonic plate boundaries.
Despite the destruction earthquakes can cause, they also drive progress in construction and emergency preparedness, showcasing the resilience and innovation of humanity.
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