Gajendra Singh Godara
Aug 7, 2025
15
mins read
Why in the News?
A powerful 8.8 magnitude earthquake struck off the coast of Russia’s Kamchatka Peninsula, leading to widespread tsunami warnings across the Pacific.
The quake, centered 119 km southeast of Petropavlovsk-Kamchatsky at a shallow depth of 19.3 km, was initially reported as 8.0 but later upgraded. It was followed by a strong 6.9 aftershock.
This marks the strongest global quake since Japan’s devastating 9.0 magnitude earthquake in March 2011 that triggered the Fukushima nuclear disaster.

Meaning of Tsunami : Tsunamis are massive ocean waves triggered by sudden underwater disturbances – most often a strong earthquake, but sometimes a volcanic eruption or underwater landslide. These waves radiate outward at jet-plane speeds across entire ocean basins. The Pacific “Ring of Fire” (aka the Circum-Pacific Belt) is a 40,000+ km long seismic zone with over 750 active/dormant volcanoes and about 90% of Earth’s largest earthquakes. As tsunamis approach shallow coastal waters, the sea floor forces the wave crests closer together and dramatically amplifies their height. Early warning systems (e.g. the Indian Ocean tsunami warning system) and public education are crucial for timely evacuations to save lives when these rare but devastating waves strike.

The Pacific Ring of Fire is a horseshoe-shaped zone of intense tectonic activity encircling the Pacific Ocean. It includes convergent plate boundaries like the Pacific–North America (Aleutian Islands), Pacific–Eurasia (Japan Trench), Nazca–South America (Andes), and Cocos–North America (Middle America Trench) regions. Subduction of oceanic plates (e.g. Pacific Plate under Eurasia/Philippine Plate, Nazca Plate under South America) forms deep trenches and volcanic island arcs.
Volcanic belts: The Ring of Fire contains roughly 750 active or dormant volcanoes (about two-thirds of all volcanoes on Earth). One example is the Trans-Mexican Volcanic Belt (in central Mexico), which formed where the Cocos (and Rivera) Plate subducts beneath the North American Plate.
Earthquake zones: About 80–90% of the planet’s largest earthquakes occur along this seismic belt. It touches countries on both sides of the Pacific: e.g. USA, Mexico, Peru, Chile in the Americas and Japan, Philippines, Indonesia, New Zealand, Russia, Australia on the Pacific Rim. (These “Pacific Ring of Fire countries” are therefore highly earthquake- and tsunami-prone.)
Table of content
Origin: Tsunamis are caused by sudden disturbances such as undersea earthquakes, volcanic eruptions, landslides, or meteorite impacts—common around the Ring of Fire in the Pacific Ocean.
Shallow-Water Waves: Despite forming in deep seas, tsunamis behave as shallow-water waves due to their extremely long wavelengths (100–500 km).
High Speed: In deep ocean waters, tsunamis can travel at jet-like speeds of 800–890 km/h.
Low Profile at Sea: Their wave height is often less than 1 meter in open ocean, making them difficult to detect visually.
Shoaling Effect: As tsunamis approach coastlines, speed reduces but wave height can exceed 30 meters, leading to severe coastal damage.
Multiple Waves: Tsunamis arrive as a series of waves; the first is rarely the strongest, adding to unpredictability.
Long Period: Wave intervals range from 10 minutes to 2 hours.
Global Reach: Tsunamis can cross entire ocean basins, retaining energy over long distances.
Natural Warnings: Receding water, strange sea sounds, or coastal tremors may signal an approaching tsunami.

Undersea Earthquakes: The most frequent trigger—typically occurring at tectonic plate boundaries such as subduction zones (e.g. along the Ring of Fire). A shallow (<70 km) earthquake of magnitude >6.5 that displaces the seafloor vertically generates a tsunami.
Volcanic Eruptions: Powerful eruptions—like the 1883 Krakatoa event—can collapse volcanic structures and displace vast water volumes, creating devastating tsunamis.
Landslides: Either coastal or submarine landslides, often quakes-induced, forcefully push water and trigger tsunamis.
Asteroid or Meteor Impacts: Though extremely rare, large impacts in oceans can displace massive water columns, leading to catastrophic tsunamis.
Other Triggers: Events like glacial calving (in polar regions) or even significant underwater explosions can displace water and form tsunami-like waves.
These causes underscore why tsunamis remain one of the most powerful and destructive natural phenomena, particularly around the highly seismic Pacific Ring of Fire.
Tectonic (Earthquake) Tsunami: Caused by sudden fault slip on the ocean floor – the most common and often most destructive type.
Volcanic Tsunami: Generated by volcanic activity (eruption, collapse, pyroclastic flow entry into water).
Landslide Tsunami: Produced when huge landslides (underwater or from a shore) displace water.
Meteorological Tsunami (Meteoric): Very rare tsunamis from asteroid impacts or exceptional atmospheric pressure waves.
Classification by Reach: Tsunamis are also described as local (hitting nearby coasts within minutes) or distant/tele-tsunami (travelling across an ocean to strike faraway shores hours later).
Pacific Basin Coasts: Western Pacific nations (Japan, Indonesia, Philippines, Taiwan) and eastern Pacific coasts of the Americas (USA, Mexico, Peru, Chile) lie on active subduction zones. For example, after the 2025 Kamchatka quake, Pacific Tsunami Warning Centre alerts were issued from Hawaii to New Zealand and as far as Japan, Chile and the US West Coast.
Indian Ocean Rim: Countries like Indonesia, India, Sri Lanka, Thailand, the Maldives and even eastern Africa face tsunami risk (as tragically shown by the 2004 Indian Ocean tsunami that killed ~220,000 people across 11 nations). An Indian Ocean Tsunami Warning System now covers this basin.
All Ocean Basins: While the Pacific sees the most frequent and largest tsunami events, smaller tsunamis can and do occur in the Atlantic, Mediterranean and Arctic oceans. In general, any region near an active seismic or volcanic zone (or steep underwater slopes) should maintain tsunami awareness.
Key Hotspots: U.S. West Coast (Cascadia subduction), South American Pacific coast, and Pacific Island chains (like Alaska, Philippines) are all high-risk. Some typically “safer” coasts (e.g. the Indian west coast) have lower frequency but are not immune. Coastal communities worldwide need to consider regional hazard assessments.
Early Warning Networks
Global systems continuously monitor seismic activity and ocean levels. For example, the Pacific and Indian Ocean warning centers use seismic and tide-gauge/buoy data to detect tsunami-generating quakes. When a potential tsunami is detected, alerts are broadcast via sirens, emergency radio/TV, and mobile notifications. (Hawaii’s emergency managers, for instance, blasted SMS/text alerts and sirens before a 2025 Pacific tsunami, evacuating residents.)
Alert Levels:
Official tsunami alerts are tiered.
Tsunami Warning (or “Threat") means widespread flooding is expected or occurring – immediate evacuation to high ground is advised.
Tsunami Advisory indicates strong currents or dangerous waves – people should stay out of the water and away from the coast.
Tsunami Watch means a tsunami is possible, so communities should prepare. These protocols (e.g., NOAA’s warning/advisory/watch definitions) help prevent confusion.
Natural Warning Signs:
Coastal residents should also recognize natural tsunami cues:
a strong coastal earthquake felt near the ocean
a sudden and unusual retreat of the sea
a loud roaring sound from the ocean can all precede an imminent wave
For example, historical accounts (like a 4th-century AD Mediterranean tsunami) describe the sea “drawn back” and exposing the seabed before the first wave struck.
Community Preparedness:
Education and drills
Regular evacuation exercises and mark high-ground routes on beaches in tsunami prone countries
Designated tsunami evacuation shelters in Coastal zones
posted warning signs. Investment in resilient infrastructure
such as reinforced sea walls
building codes for coastal structures
Scale of Destruction: Tsunamis can range from minor, imperceptible occurrences to catastrophic events. For example, small tsunamis caused by minor underwater disturbances often go unnoticed unless monitored.
Human Toll: The 2004 Indian Ocean tsunami claimed over 225,000 lives across 14 countries, while the 2011 Tōhoku tsunami in Japan caused nearly 16,000 deaths and forced over 300,000 people into temporary displacement.
Infrastructure Collapse: Coastal infrastructure-including homes, bridges, and roads-is often obliterated. The 2011 Japan event led to unprecedented damage valued in hundreds of billions of dollars. For example, in the 2025 Kamchatka event, flooding in Russia’s Kuril Islands caused damage to homes and facilities. In Japan, even a 0.6 m wave led to the evacuation of nearly 2 million people.
Environmental Degradation: Tsunamis disrupt ecosystems by destroying coral reefs, mangroves, and wetlands. Saltwater inundation also contaminates freshwater systems and soil, severely affecting agriculture and biodiversity.
Secondary Hazards: Post-tsunami effects include hazardous material leaks, fires, and cascading disasters. The Fukushima Daiichi nuclear meltdown following the 2011 Japan tsunami exemplifies such compound calamities.
Health and Psychological Impact: Victims often face waterborne illnesses, overwhelmed health services, and long-lasting mental health issues such as PTSD. Survivors struggle with loss of property, routine, and emotional trauma.
Service Disruptions & Displacement: Essential services-electricity, water, and communication-are typically knocked out, while widespread displacement strains relief and rehabilitation systems.
Global Ripple Effects: Major tsunamis such as the ones in the Indian Ocean and Japan had far-reaching impacts on global trade, tourism, and supply chains, especially when key ports are disrupted.
Comprehensive Mitigation Approach
Reducing tsunami risk relies on layered protection: early warning systems, well-mapped evacuation routes, community education, and natural barriers such as mangroves, coral reefs, and dunes to absorb wave energy.Global Warning Networks
Pacific Tsunami Warning System (PTWS): Overseen by UNESCO/IOC via ICG/PTWS, employing DART buoys and seismic sensors across Pacific ‘Ring of Fire’ nations.
Indian Ocean Tsunami Warning & Mitigation System (IOTWMS): Established post‑2004 tsunami, operational since 2013, with Regional Tsunami Watch Providers (TSPs) in India, Indonesia, and Australia delivering alerts to 28 member countries.
India’s National Mechanism: The Indian Tsunami Early Warning Centre (ITEWC) at INCOIS, Hyderabad, acts as a Tsunami Service Provider under IOTWMS.
Education & Preparedness
Public awareness-through drills, signage, media, and community workshops—boosts response efficacy in nations like Japan. Natural signs such as receding water also help save lives quickly.
Emerging Technology Enhancements
India is piloting a smart underwater cable system along the Andaman–Nicobar subduction zone, equipped with sensors like bottom-pressure recorders and seismometers to improve detection reliability.
A horseshoe‑shaped seismic hotspot encircling the Pacific Ocean, stretching nearly 40,000 km.
Known for intense tectonic activity—home to 90% of the world’s earthquakes and 75% of active volcanoes, due to subduction zones and plate collisions.
This dynamic zone is where most tsunamis originate, making it critically relevant to understanding the causes and effects of tsunamis.
Countries most affected include Japan, Indonesia, Chile, United States (Alaska and West Coast), and New Zealand—areas prone to earthquakes, volcanic eruptions, and tsunamis.

Question 1: The 2004 Tsunami made people realize that mangroves can serve as a reliable safety hedge against coastal calamities. How do mangroves function as a safety hedge? (UPSC Prelims 2011)
(a) The mangrove swamps separate the human settlements from the sea by a wide zone in which people neither live nor venture out.
(b) The mangroves provide both food and medicines that people are in need of after any natural disaster.
(c) The mangrove trees are tall with dense canopies and serve as an excellent shelter during a cyclone or tsunami.
(d) The mangrove trees do not get uprooted by storms and tides because of their extensive roots.
Ans: (d)
Q. How does a tsunami differ from a regular ocean wave?
A. Tsunamis result from massive water displacement-like submarine earthquakes or volcanic eruptions-travel at jet-plane speeds, and have very long wavelengths, making them far more destructive than ordinary wind-driven waves.
Q. What is the Pacific Ocean Ring of Fire, and which nations lie on it?
A. The Ring of Fire is a 40,000 km horseshoe‑shaped seismic zone around the Pacific Ocean that includes countries like Japan, Indonesia, Philippines, New Zealand, the U.S. West Coast, Canada, Russia, Mexico, Peru, and Chile.
Q. What natural warning signs precede a tsunami?
A. Strong, prolonged coastal earthquakes; sudden sea retreat exposing the seabed; and a roaring ocean sound-these are key natural alerts prompting immediate evacuation.
Q. What are the main causes of tsunamis?
A. Primary causes include undersea earthquakes in subduction zones, volcanic eruptions, and landslides. Rare triggers include asteroid impacts, underwater explosions, and glacial calving events.
Q. Why are countries along the Pacific Ocean Ring of Fire especially vulnerable to tsunamis?
A. Their location along subduction zones makes them prone to powerful earthquakes and volcanic eruptions-events that frequently initiate tsunami waves.
Tsunamis remain one of the most devastating natural hazards for coastal communities worldwide, especially around the Pacific and Indian Oceans. The Ring of Fire (Circum-Pacific seismic belt) – a 40,000 km zone of subduction – contains the majority of Earth’s active volcanoes and largest earthquakes. These tectonic processes displace vast amounts of water, creating tsunami waves that can travel across oceans. By understanding how tsunamis form (plate tectonics, earthquake mechanics, volcanic triggers) and the scale of their impacts, societies can better prepare. Cutting-edge monitoring, robust warning systems and regional cooperation are crucial. In short, informed vigilance (education, drills, and global alert networks) is essential to reduce the loss of life and property from these rare but catastrophic waves.
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