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Published July 1, 2023

Understanding Earthquakes and Tectonic Hazards

By Hannah Coe
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Tectonic hazards are natural disasters caused by movement within the Earth’s crust. This movement can occur along faults where tectonic plates meet and interact. Examples include earthquakes, caused by sudden slips along faults; volcanic eruptions, occurring when magma escapes through cracks in the Earth’s surface; and tsunamis, triggered by underwater earthquakes or volcanic activity. Understanding tectonic hazards is crucial for building resilient infrastructure and preparing communities for effective response.

What are the primary effects of an earthquake?

The primary effects of an earthquake are the immediate and direct consequences of the seismic activity. This includes ground shaking, which can lead to the collapse of buildings, bridges, and other structures; surface rupture, where the ground itself breaks apart; and landslides in hilly or mountainous regions. These primary effects can result in injury or loss of life, as well as extensive damage to property and infrastructure.

What are the secondary effects of earthquakes?

Secondary effects are the indirect consequences that follow the initial seismic event. These may include fires sparked by damaged electrical lines or gas leaks; tsunamis triggered by undersea earthquakes; flooding due to dam or levee failures; and social and economic disruption, such as loss of jobs, business closures, and displacement of communities. Secondary effects can exacerbate the challenges of recovery and reconstruction.

What damage can an earthquake do?

An earthquake can cause widespread damage to the built environment and natural landscape. Buildings may collapse or suffer structural damage; roads and bridges can crack or crumble; utility lines may be severed, leading to loss of essential services like water, electricity, and communication. In addition to physical damage, earthquakes can have lasting psychological effects on those who experience them, leading to stress, anxiety, and trauma.

What are the causes of an earthquake?

Earthquakes are caused by the sudden release of energy within the Earth’s crust, often along faults where tectonic plates meet. This release of energy can result from the movement of tectonic plates as they collide, pull apart, or slide past each other; volcanic activity; or human activities such as mining or reservoir-induced seismicity. The energy radiates outward as seismic waves, creating the ground shaking that characterizes an earthquake.

How can we prepare for an earthquake?

Preparing for an earthquake involves understanding the risks, implementing building codes and construction practices that enhance structural resilience, and developing community preparedness plans. Individuals can also take measures such as securing heavy furniture and breakable items, creating emergency supply kits, and having an evacuation plan. Public education and awareness campaigns, early warning systems, and collaboration among governments, scientists, and engineers can also contribute to a community’s readiness and ability to respond to an earthquake.

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