Earthquake Essentials
Explore how quakes start, why some regions are constantly on edge, how scientists gauge their power, and the cascading hazards that can follow.
What Causes Earthquakes?
An earthquake occurs when two blocks of the Earth suddenly slip past one another along a fault or fault plane. The surface where they slip is the fault, the below-ground starting point is the hypocenter, and the point directly above it is the epicenter.
This sudden release of energy generates seismic waves that shake the ground, sometimes causing widespread damage. Most earthquakes happen along the edges of tectonic plates, massive slabs of the Earth's crust that constantly move and interact.
The Ring of Fire and Earthquake Hotspots
80% of the world's earthquakes occur in the "Ring of Fire," a horseshoe-shaped zone around the Pacific Ocean where tectonic plates collide and grind past one another.
Countries such as Japan, Chile, the Philippines, and the western United States are especially prone to seismic activity because of their location along this volatile boundary. Japan records more earthquakes than any other country.
Measuring Earthquake Strength
Modern seismologists use the Moment Magnitude scale to measure the energy released by an earthquake, replacing the older Richter scale for greater accuracy.
The strongest earthquake ever recorded was a magnitude 9.5 event in Chile in 1960 that lasted about 10 minutes and triggered devastating tsunamis. Quakes below magnitude 2.5 are rarely felt, while events above 7.5 can cause severe destruction near populated areas.
Secondary Hazards: Tsunamis, Landslides, and Fires
- Tsunamis: Undersea quakes displace seawater, sending waves racing across oceans at over 600 mph before flooding coastlines.
- Landslides: Strong shaking can destabilize slopes, as seen in the 2008 Sichuan earthquake in China, which triggered massive failures.
- Fires: Ruptured gas lines and damaged electrical systems can ignite blazes, like the 1906 San Francisco earthquake where fires caused more deaths than the shaking.