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The Seismic Lottery: Why Infrastructure Beats Magnitude

In the seismic lottery, it's not the size of the shake that determines your fate—it's where you bought your ticket. The same magnitude earthquake can kill thousands in one country while barely making headlines in another.

April 14th, 2025: San Diego wins the seismic lottery.

A 5.2 magnitude earthquake struck near the city, yet life continued almost normally. Meanwhile, earthquakes of similar strength have devastated communities worldwide. What makes the difference? Infrastructure resilience—the ultimate lottery ticket in seismic survival.

But first, let's understand
how earthquakes actually work.

The story begins deep underground,
where immense forces have been
building for decades.

Tectonic Pressure Buildup

For years, decades, even centuries, massive tectonic plates lock together along fault lines. Stress accumulates as they attempt to move, building enormous pressure that must eventually be released.

100+ Years of Buildup
50+ km Typical Depth

Catastrophic Energy Release

When the fault finally snaps, all that stored energy is released instantaneously. Seismic waves race outward at incredible speeds, carrying energy equivalent to multiple nuclear bombs.

8 km/s Wave Speed
10¹⁶ Joules Released

How Much Energy Is That?

Use the controls to compare earthquake energy with nuclear explosions!

7.0
50
Total Energy Released 1.0 Ɨ 10¹⁵ J
Surface Impact Level Strong (5.2)
32
Hiroshima bombs (surface effect)
Each šŸ’£ = 100 bombs

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