Understanding Earthquakes Lesson: An Easy Guide

Created by ProProfs Editorial Team
The ProProfs editorial team is comprised of experienced subject matter experts. They've collectively created over 10,000 quizzes and lessons, serving over 100 million users. Our team includes in-house content moderators and subject matter experts, as well as a global network of rigorously trained contributors. All adhere to our comprehensive editorial guidelines, ensuring the delivery of high-quality content.
Learn about Our Editorial Process

Lesson Overview

Earthquakes are natural events that cause the ground to shake. They occur when energy is released due to movements within the Earth's crust. These movements are caused by tectonic plates shifting, colliding, or sliding past each other. 

Some earthquakes are too small to feel, while others can be powerful enough to change landscapes. In this lesson, we will explore what earthquakes are, what causes them, where they happen most often, and how to stay safe when one occurs.

The Structure of the Earth

To understand earthquakes, we need to understand the Earth's layers. The Earth is made up of four layers:

LayerDescription
CrustThe thin outer layer where we live. It is broken into tectonic plates.
MantleA thick layer of hot, flowing rock beneath the crust. It helps move the plates.
Outer CoreA layer of liquid metal that creates Earth's magnetic field.
Inner CoreA dense, solid metal center, hotter than the sun's surface.

These layers play a role in plate tectonics, which is responsible for earthquakes.

Tectonic Plates and Earthquakes

The Earth's crust is not a single solid piece; it is broken into tectonic plates. These plates move slowly over time, and their movement causes earthquakes. Most earthquakes occur at plate boundaries, where plates interact in different ways:

Type of Plate MovementDescription
Convergent BoundaryPlates push against each other, causing mountains or deep-sea trenches.
Divergent BoundaryPlates move apart, forming new crust.
Transform BoundaryPlates slide past each other, creating friction and sudden movement.

One of the most earthquake-prone regions in the world is the Ring of Fire, which surrounds the Pacific Ocean and includes countries like Japan, Chile, and the U.S. west coast.

How Earthquakes Happen

When tectonic plates move, they sometimes get stuck due to friction. As pressure builds up, the energy is suddenly released, causing an earthquake. The place underground where the earthquake starts is called the focus, and the point directly above it on the surface is called the epicenter.

Seismic Waves

During an earthquake, energy travels in waves through the ground. There are three main types of seismic waves:

Wave TypeDescription
Primary (P) WavesTravel fastest, moving back and forth. Can move through solid and liquid layers.
Secondary (S) WavesMove side to side, slower than P-waves, and only travel through solids.
Surface WavesMove along the Earth's surface, causing the most damage.

Take This Quiz:

Effects of Earthquakes

Earthquakes can cause damage to buildings, roads, and bridges. In some cases, they trigger landslides, tsunamis, or fires due to broken gas lines. Scientists measure earthquake strength using the Richter Scale or Moment Magnitude Scale (Mw). A higher magnitude means a stronger earthquake.

MagnitudeEffect
Below 3.0Usually not felt by people.
3.0 - 4.9Felt, but rarely causes damage.
5.0 - 6.9Can cause significant damage to buildings.
7.0 and aboveMajor earthquakes that can destroy cities.

Foreshocks, Mainshocks, and Aftershocks

Earthquakes can occur in sequences:

  • Foreshocks: Small tremors before the main earthquake.
  • Mainshock: The largest earthquake in a sequence.
  • Aftershocks: Smaller tremors that follow the mainshock.

Not all earthquakes have foreshocks, but aftershocks are common and can last days or weeks.

How to Stay Safe During an Earthquake

If you experience an earthquake, follow the Drop, Cover, and Hold On method:

  1. Drop to the ground to prevent falling.
  2. Cover your head and neck under a sturdy table or desk.
  3. Hold On until the shaking stops.

If outside, move away from buildings and trees. If driving, stop safely and stay inside the vehicle.

Interactive Learning Activities

1. Earthquake Simulation with Crackers

  • Use two crackers on a plate with soft frosting underneath to represent tectonic plates.
  • Move them toward, apart, and past each other to simulate different plate movements.
  • Observe how the frosting acts like the mantle, letting the plates move.

2. Build an Earthquake-Proof Structure

  • Use straws, tape, and marshmallows to build a structure.
  • Shake the table and observe which designs withstand the motion best.
  • Learn why engineers design flexible buildings in earthquake-prone areas.

3. Earthquake Location Mapping

  • Use a world map to identify major earthquake-prone zones.
  • Look at recent earthquakes and discuss why they occurred in certain locations.

Practice Questions

Try answering these questions to review what you learned:

  1. What are the four main layers of the Earth?
  2. What is the Earth's outer shell made of?
  3. What happens when two plates push against each other?
  4. Where do most earthquakes occur?
  5. What should you do during an earthquake?

Take This Quiz:

Rate this lesson:

Back to Top Back to top
Advertisement
×

Wait!
Here's an interesting quiz for you.

We have other quizzes matching your interest.