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What to Do After an Earthquake: Essential Safety Steps Explained

What to Do After an Earthquake: Essential Safety Steps Explained

by Gelogia Team | May 16, 2026 | Earthquakes

When the shaking stops, the danger may not be over. After an earthquake, people may face: aftershocks damaged buildings gas leaks fires power outages blocked roads The minutes and hours after an earthquake are extremely important. Knowing what to do afterward can help...
What to Do During an Earthquake: Essential Safety Actions Explained

What to Do During an Earthquake: Essential Safety Actions Explained

by Gelogia Team | May 16, 2026 | Earthquakes

Earthquakes happen suddenly and often without warning. In just a few seconds: buildings may shake violently objects can fall power systems may fail roads and structures may become dangerous Knowing what to do during an earthquake can greatly reduce injuries and...
Earthquake Intensity Scale Comparison: Why Magnitude and Shaking Are Different

Earthquake Intensity Scale Comparison: Why Magnitude and Shaking Are Different

by Gelogia Team | May 16, 2026 | Earthquakes

Many people think earthquake magnitude and earthquake intensity mean the same thing. But they are actually very different. Magnitude measures the total energy released by an earthquake. Intensity measures how strongly the earthquake is felt at a specific location....
Earthquake Energy Release Explained: How Earth Stores and Releases Seismic Power

Earthquake Energy Release Explained: How Earth Stores and Releases Seismic Power

by Gelogia Team | May 15, 2026 | Earthquakes

Earthquakes are giant releases of stored energy deep underground. For years — sometimes centuries — tectonic plates slowly push, pull, or grind against each other. During this time: rocks bend faults lock stress builds underground Eventually, the rocks can no longer...
Foreshocks vs Mainshock vs Aftershocks: How Earthquake Sequences Work

Foreshocks vs Mainshock vs Aftershocks: How Earthquake Sequences Work

by Gelogia Team | May 15, 2026 | Earthquakes

Many earthquakes do not happen alone. Instead, they occur as part of a sequence involving: smaller earthquakes before the main event one major earthquake continued shaking afterward These stages are called foreshocks, mainshock, and aftershocks. Understanding these...
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