When the Earth Shakes

A free interactive lesson on earthquakes for Class 5 — how Earth's tectonic plates move and cause earthquakes, what seismic waves are, how the Richter scale measures magnitude, and Drop Cover Hold On safety. Based on NCERT Class 5 Earth and Weather. Includes quiz.

Class 5 ScienceClass 5 / Grade 5Ages 7–10
Lesson
🌍 When the Earth Shakes
The ground shakes — but why?CoreCrust (thin layer)Mantle (hot rock)The Earth's crust isbroken into giantplates that move.When they slip →earthquake! 🌍

Earth's surface looks solid and still — but it is actually broken into giant pieces called tectonic plates, floating on a layer of hot, slow-moving rock called the mantle. When these plates move — colliding, separating, or grinding past each other — the ground shakes. That's an earthquake.

Earth's structure and tectonic plates

Earth is not a solid ball — it has layers. The outermost layer, the crust, is broken into about 15 large pieces called tectonic plates. These plates float on the semi-molten mantle below and move very slowly — about 2–5 cm per year, roughly the speed your fingernails grow. Where plates meet are called plate boundaries, and these are where most geological activity happens.

What causes earthquakes

Earthquakes happen when tectonic plates move suddenly. At plate boundaries, three things can happen:

  • Collision (convergent boundary) — two plates crash into each other. One may be pushed under the other (subduction) or the collision may push up mountain ranges like the Himalayas.
  • Separation (divergent boundary) — two plates pull apart, creating rifts and allowing magma to rise from the mantle. The Mid-Atlantic Ridge is an example.
  • Sliding (transform boundary) — plates slide horizontally past each other, like the San Andreas Fault in California. Friction builds up and releases suddenly as an earthquake.

The point underground where the earthquake starts is the focus; the point on the surface directly above is the epicentre, where shaking is usually strongest.

Measuring earthquakes

Earthquakes are measured using a seismograph — an instrument that records the vibrations (seismic waves) travelling through the ground. The Richter scale measures earthquake magnitude — each whole number increase represents 10× more ground motion and about 31× more energy. A magnitude 2 earthquake is barely felt; magnitude 6 can damage buildings; magnitude 9 is catastrophic.

Earthquake safety — Drop, Cover, Hold On

The safest action during an earthquake is Drop, Cover, Hold On:

  • Drop — get onto your hands and knees immediately. This protects you from being knocked over and lets you move if needed.
  • Cover — get under a sturdy table or desk. If there's no cover, cover your head and neck with your arms. Do NOT stand in a doorway — it's a myth that doorways provide protection.
  • Hold On — stay under cover and hold on until shaking stops. After it stops, move carefully and watch for falling objects.

Frequently asked questions

What causes earthquakes?

Earthquakes are caused by the sudden movement of tectonic plates — the large pieces that make up Earth's crust. Plates collide, separate, or slide past each other. When plates get stuck and then suddenly slip, the released energy travels as seismic waves, causing shaking.

What is the Richter scale?

The Richter scale measures the magnitude (size) of an earthquake. Each whole number increase means 10× more ground shaking and about 31× more energy. Earthquakes below 3 are usually not felt; above 6 can cause significant damage.

What should you do during an earthquake?

Drop (get on hands and knees), Cover (get under a sturdy table or protect your head with your arms), Hold On (stay under cover until shaking stops). Move away from windows, heavy furniture, and exterior walls.

Why does India experience earthquakes?

India sits on the Indian tectonic plate, which is slowly colliding with the Eurasian plate — a collision that created the Himalayas. This ongoing collision causes frequent earthquakes in northern and northeastern India. The Andaman Islands are also highly seismic due to subduction zone activity.

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