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Earthquakes, Tsunamis and Volcanic Activity

Earthquakes, tsunamis, and volcanic eruptions are among the most destructive geophysical events. This article covers how they occur and how their risk is assessed.

Augustine Volcano, Alaska, erupting with an ash and gas plume
Augustine Volcano, Alaska, during its 2006 eruptive phase. Photo: Cyrus Read, USGS, public domain, via Wikimedia Commons.
Map of the Pacific Ring of Fire showing major trenches and volcanoes
The Pacific Ring of Fire, where roughly 90% of the world’s earthquakes and two-thirds of its active volcanoes are concentrated. Map: Gringer and contributors, public domain, via Wikimedia Commons.
MCQ Questions
World Geography
Earthquakes, Tsunamis and Volcanic Activity
Related hazards, driven by the same tectonic processes
Key Distinction
Hazard vs. Disaster
A disaster is a hazard striking a vulnerable population.
Sudden Release
Earthquakes
Fault-line stress releases as seismic waves.
Often Undersea
Tsunamis
Usually triggered by a large undersea earthquake.
Along Belts
Volcanic Eruptions
Molten material escapes along volcanic belts.
📑 Contents
✊ Must Know
How Earthquakes and Volcanoes Happen
  • A hazard is a potential source of danger. A disaster is what happens when a hazard actually strikes a vulnerable population. The two aren’t the same thing.
  • Forces The lithosphere is broken into several plates, called lithospheric plates, that move a few millimetres each year because of molten magma moving inside the earth. Forces acting in the interior of the earth are endogenic; forces working on the surface are exogenic. Sudden endogenic events like earthquakes and volcanoes cause mass destruction.
  • Focus, Epicentre & Scale The place in the crust where an earthquake starts is its focus. The point on the surface directly above it is the epicentre. Earthquakes are recorded by a seismograph, and their magnitude is measured on the Richter scale. A reading over 5.0 causes damage, 6.0+ is very strong, and 7.0 is a major earthquake.
  • Earthquakes occur when built-up stress along fault lines releases suddenly, generating seismic waves that travel through the Earth.
  • A tsunami is typically triggered by a large undersea earthquake, though volcanic eruptions and landslides can also trigger one.
  • Volcanic eruptions occur when molten material and gases escape from beneath the Earth’s crust, often concentrated along specific volcanic belts.
  • Volcanic eruptions release several distinct products together. These include pyroclastic debris (fragmented rock ejected by the blast), ash and dust, and gases like sulphur compounds and nitrogen compounds.
📘 Good to Know
Measuring and Managing the Risk
  • Risk assessment for geophysical hazards combines the likelihood of an event with the vulnerability of the population and infrastructure exposed to it.
  • Seismic zones vary in risk across India and the world. The same magnitude earthquake can cause very different levels of damage, depending on where it strikes.
  • India’s Zoning System India is divided into four seismic zones, II to V, based on earthquake risk. Zone V is the highest-risk band, covering the Himalayan belt, the north-east, Kutch and the Andaman & Nicobar Islands, while Zone II is the least active.
  • Early warning mechanisms for tsunamis, developed after major disasters like the 2004 Indian Ocean tsunami, aim to give coastal populations critical minutes to evacuate.

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🌟 Great to Know
Hazard vs. Disaster, and Shared Origins
  • The hazard-versus-disaster distinction matters for policy, not just terminology. A hazard is often unavoidable, since it stems from natural processes. A disaster’s scale, though, depends heavily on human factors like building codes, preparedness, and early warning systems. Disaster impact is partly a policy choice, not purely a natural outcome.
  • The same underlying tectonic activity that makes a region earthquake-prone often also makes it volcanically active. Both processes are frequently driven by the same plate boundary dynamics, like the Pacific “Ring of Fire.”
  • Tsunami early-warning systems illustrate a broader principle in disaster risk reduction. Since the underlying hazard often can’t be prevented, investment increasingly shifts toward reducing the time between detection and public warning. That gap is where lives are actually saved or lost.
📰 Current Affairs
Current Affairs
📝 Previous Year Questions
P Waves vs. S Waves: The Real 2023 Question
  • P waves win Primary (P) waves are the fastest seismic waves and always reach a recording station’s seismograph before Secondary (S) waves.
  • Motion type P waves are compressional, so particles vibrate back and forth along the same direction the wave travels. S waves are shear waves, so particles vibrate at right angles to that direction instead.
  • Answer: (c) Both statements are correct.
  • View this question on the full 2023 paper →

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