The moving ground
The Nazca plate slides under South America at about the speed a fingernail grows, and every so often it lets go. Chile has been measuring what happens next for longer than almost anyone.
Why here
What do you learn in a country that moves?
The mechanism is easy to state and brutal to live through: two locked plates store strain for decades and give it back in minutes. What makes Chile different is not that it shakes — half the Pacific rim shakes — but the scale and the consistency. The largest earthquake ever recorded by an instrument happened here, and every aftershock of the country’s seismic history since is data that simply does not exist elsewhere.
That makes the country an involuntary laboratory of structural engineering. A Chilean way of measuring how violent the shaking is — Arias intensity, published in 1970 — is written into engineering codes around the world, and base isolation stopped being exotic here long ago: it is routine in hospitals and tall buildings.
And the experiment is not optional. Every building is a specimen, and after each large earthquake the code changes, because the whole country has just run the full-scale test no laboratory could afford.
The numbers, with their sources
the largest earthquake ever recorded by an instrument anywhere: Valdivia, 22 May 1960.
What we have on this
Scientists
Concepts, explained with animation
In depth
If you work with any of this
Instruments, fieldwork, a programme that needs one of these conditions, or simply a story that is better told from here. That is the conversation we are interested in.
What we can do together →