Earthquake Hazards and Damage — Reading Comprehension

Earthquakes are sudden movements of the Earth's surface that can cause widespread damage and danger. These natural events are important to study because they threaten lives, property, and infrastructure in many parts of the world. Understanding earthquake hazards helps scientists, engineers, and communities prepare and reduce risk. This passage explores the main hazards caused by earthquakes, explains why they occur, and examines their impacts using real-world examples.

Ground Shaking and Surface Rupture

The most immediate hazard from an earthquake is ground shaking. The intensity of shaking depends on the earthquake's magnitude (the amount of energy released), the distance from the earthquake's center, and the local geology. For example, areas with soft sediments can experience more intense shaking because the ground acts like a sponge, amplifying the waves. Sometimes this causes liquefaction, when the ground temporarily behaves like a liquid, causing buildings and roads to sink or tilt. Another hazard is surface rupture, where the ground splits open along a fault line, breaking roads, pipes, and structures above.

Landslides, Tsunamis, and Fires

Earthquake shaking can trigger landslides on unstable slopes, especially in mountains or areas with loose soil. These landslides can bury homes and block roads, making rescue and recovery difficult. Under the ocean, earthquakes can cause tsunamis: giant waves formed when the seafloor suddenly moves. Tsunamis travel rapidly across oceans, flooding coastlines and causing destruction far from the earthquake's origin. Fires are another major hazard, often started by ruptured gas lines or broken electrical wires during an earthquake. Fires can spread quickly if water lines are damaged and firefighters cannot respond.

Building Collapse, Infrastructure Damage, and Aftershocks

The type and age of construction play a major role in earthquake damage. Older or poorly engineered buildings are more likely to collapse, trapping people inside. Earthquakes also damage infrastructure like bridges, roads, and utilities (electricity, water, sewage). After the main shock, aftershocks—smaller earthquakes—can continue for days or weeks, causing more damage and danger. Historic examples show the range of earthquake impacts: the 1906 San Francisco earthquake caused fires that destroyed much of the city; the 1964 Alaska earthquake led to landslides and tsunamis; the 2010 Haiti earthquake had massive building collapses; and the 2011 Japan earthquake triggered a devastating tsunami.

Understanding how earthquakes cause multiple hazards helps communities improve safety through engineering, emergency planning, and education. By studying past events and local geology, scientists can identify high-risk areas and develop better ways to reduce earthquake damage. These efforts support the broader scientific principle that human actions and natural systems are interconnected.

Interesting Fact: The energy released by a magnitude 8 earthquake can be over 1,000 times greater than a magnitude 6 earthquake, showing how small differences in magnitude can cause huge changes in damage.

What is the primary hazard caused directly by an earthquake?

How does local geology affect earthquake damage?

What is liquefaction?

Which type of hazard can bury homes and block roads after an earthquake?

In the passage, what does the word 'infrastructure' mean?

Why are aftershocks dangerous?

Which historical earthquake caused a major tsunami and nuclear disaster?

If a city is built on soft, wet soil, what is one likely effect during an earthquake?

True or False: Fires after earthquakes are often caused by broken gas or electrical lines.

True or False: All earthquakes cause tsunamis.