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The NPR article discusses the science behind aftershocks following earthquakes, with a particular focus on the recent earthquake in Turkey. The article explains that aftershocks occur because the Earth's crust is not perfectly elastic, and earthquakes release energy that can cause additional shaking in the surrounding area. Scientists use statistical models to predict the likelihood and intensity of aftershocks, but they cannot predict exactly when or where they will occur.
The article notes that aftershocks can be just as dangerous as the initial earthquake, and they can continue for weeks, months, or even years after the initial event. Scientists use a variety of techniques to monitor aftershocks, including seismometers and GPS sensors, and they use this data to update their models and better understand the underlying physics of earthquakes.
The article concludes by noting that earthquakes are a natural part of the Earth's geology, and that humans must learn to coexist with them. Scientists and engineers can help reduce the risk of earthquakes through better building codes and infrastructure, but ultimately, earthquakes will continue to occur. By better understanding the science of aftershocks, however, we can prepare for them and minimize their impact on our communities.
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