Previous research has found that Earth mostly rebounds after quakes, with blocks of the world's crust elastically springing back, over the course of months to decades, to the way they initially were.
Such rebounding was first seen after investigations of the devastating 1906 San Francisco temblor that caused destruction of more than 80 per cent of the city, website 'OurAmazingPlanet' reported.
The rebound is well-documented now by satellite-based Global Positioning System (GPS) systems that monitor Earth's movements.
However, structural geologist Richard Allmendinger of Cornell University and his colleagues in the new study found that major earthquakes of magnitude 7 or greater apparently caused the crust in northern Chile to crack permanently.
In northern Chile, "the driest place on Earth, we have a virtually unique record of great earthquakes going back a million years," Allmendinger said.
Whereas most analyses of ancient earthquakes only probe cycles of two to four quakes, "our record of upper plate cracking spans thousands of earthquake cycles," he noted.
The record of the vast number of earthquakes captured in northern Chilean rocks allowed the researchers to examine their average behaviour over a much longer period of time, which makes it easier to pick out any patterns.
The crust may behave less elastically than previously thought.
"It is only in a place like the Atacama Desert that these cracks can be observed - in all other places, surface processes erase them within days or weeks of their formation, but in the Atacama, they are preserved for millions of years," Allmendinger said.
The study was published in the journal Nature Geoscience.
