Understanding Earthquakes and Prediction Challenges

Floods in Europe

Hurricanes in the Caribbean

Wildfires in Australia

Earthquakes in Turkey and Syria

Epicenter

Fault line

Hypocenter

Seismic zone

Stress overcoming friction

Tectonic plate cooling

Meteor impact

Volcanic eruption

They are where tectonic plates meet

They are areas of high volcanic activity

They have the most human activity

They are the oldest parts of the Earth

They cause more damage

They are less frequent

They are easier to predict

They cause less surface shaking

Too many earthquakes occur simultaneously

Inconsistent historical data

Faults are silent until they slip

Lack of technology

Early warnings are only for aftershocks

Predictions are based on animal behavior

Early warnings are issued after an earthquake starts

Predictions are more accurate

Using animal behavior

AI detection of subtle signals

Increased seismic noise

More frequent drilling

By predicting the next earthquake

By assessing building damage

By stopping aftershocks

By reducing seismic noise

Predicting exact times and locations

Building earthquake-resistant infrastructure

Relying on animal behavior

Using historical data for predictions