
Tsunamis are among the most destructive natural forces on Earth. What starts as a barely noticeable disturbance in the deep ocean can turn into towering waves that crash onto coastlines with devastating power. But what exactly causes a tsunami, and how do these waves grow so large near the shore? Let’s explore the science behind it.
A tsunami is a series of sea waves caused by a sudden and massive disturbance beneath the ocean’s surface. These events are most commonly triggered by underwater earthquakes but can also result from volcanic eruptions, undersea landslides, or even meteorite impacts.
If you could drain the oceans, you would see that the Earth’s crust is made up of giant interlocking pieces called tectonic plates. These plates float on the semi-molten layer of the Earth and are in constant motion due to convection currents in the mantle.
There are seven major tectonic plates, and when these plates interact, they cause earthquakes and volcanic activity. One common interaction is subduction, where one plate slides beneath another. Over time, stress builds up in the upper plate. When the stress is released, it pushes the seabed upward, displacing an enormous volume of water and generating a tsunami.

Subduction zones are the primary locations for tsunami-triggering earthquakes. In places like the Japan Trench and the Chile Peru Trench, strain energy accumulates for decades or even centuries. When released, this energy causes a sudden uplift in the ocean floor, producing a fast-moving tsunami wave.
Although the wave can travel at more than 200 kilometers per hour, it often passes unnoticed in deep waters due to its small height and long wavelength.
As the tsunami wave approaches land, the ocean depth decreases. This change in depth causes the wave to slow down. Since the wave’s energy remains constant, the wave height increases dramatically. This process is known as wave shoaling.
As a result, a wave that was barely visible in the open sea can grow into a massive wall of water when it nears the shore. This is when tsunamis become truly destructive.
A common misconception is that the water itself moves across the ocean. In reality, water particles mostly move in place, oscillating vertically. However, when the wave’s height increases near land, the energy becomes destructive. The wave crashes onto the shore, even though individual water particles are not moving forward in a horizontal direction.
On December 26, 2004, one of the deadliest tsunamis in recorded history struck the coasts of several countries bordering the Indian Ocean. It was caused by a powerful earthquake measuring between 9.1 and 9.3 in magnitude, off the coast of Sumatra, Indonesia.
This earthquake occurred because the Indian tectonic plate was forced under the Burma plate, causing the seafloor to rise and displace massive amounts of water. The energy released was equivalent to over 23 thousand atomic bombs.

Waves traveled at speeds of up to 800 kilometers per hour, reaching some coastlines in minutes and others, like those in India and Africa, hours later.
On July 30, 2025, at 11:24 AM local time, a massive magnitude 8.8 earthquake struck just off the eastern coast of Russia’s Kamchatka Peninsula. The powerful megathrust quake occurred about 119 kilometers southeast of the city of Petropavlovsk-Kamchatsky, shaking the far eastern region with intense force.
Although earthquakes are the leading cause, other natural events can also trigger tsunamis:
Volcanic eruptions beneath the sea can displace water and generate powerful waves.
Underwater or coastal landslides can push large volumes of water outward.
A massive meteorite impact in the ocean could trigger a rare but catastrophic tsunami event.
One example of such a geological tsunami is the one caused by a volcanic collapse in Indonesia, where a volcano exploded and pushed out enough water to generate large waves.
A widely observed warning sign is the sudden and dramatic retreat of the shoreline. This can happen when the trough of the tsunami wave reaches the coast first, pulling water away from the land. A few seconds later, the crest of the wave arrives, often with deadly force.
However, not all tsunamis begin with a receding shoreline. In some cases, the crest may arrive first without warning.
Tsunamis are most often caused by underwater earthquakes, but volcanic eruptions, landslides, and meteorite impacts can also lead to their formation.
As the waves move into shallow waters, their speed decreases and their height increases. This transformation is called wave shoaling.
Tsunami waves can travel as fast as 800 kilometers per hour in deep water, similar to the speed of a jet aircraft.
While earthquakes cannot be predicted, modern tsunami warning systems can detect undersea earthquakes and issue alerts to potentially affected regions.
No, tsunamis can also be caused by volcanic eruptions, landslides, and in very rare cases, meteorite impacts.
Tsunamis are powerful reminders of the dynamic and ever-changing nature of our planet. Caused by the shifting of Earth’s tectonic plates and other natural forces, they begin silently but can end with unimaginable devastation. Understanding how they form helps us better prepare and respond when nature unleashes its fury.
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Dony Garvasis is the founder of Search Ethics, a platform dedicated to transparency, authenticity, and ethical digital practices. With over six years of experience in SEO and digital marketing, I provide expert content on automobiles, Artificial intelligence, technology, gadgets, science, tips, tutorials and much more. My mission is simple: Ethical Search, Genuine Results! I will make sure people everywhere get trustworthy and helpful information.






