The latest earthquake off Japan’s east coast was an ominous reminder of the 2011 Fukushima disaster. But despite a technical hitch at one of Fukushima’s other reactors, there was no repeat this time.
Japan’s response to a tsunami threat following major earthquake shows it has learned much from past events, including the deadly quake and tsunami that disabled the Fukushima nuclear power plant.
Potentially deadly and dangerous earthquakes can strike at any time. But can authorities get some early warning from monitoring the hundreds of small quakes that usually go unnoticed?
A new study of the 2011 Christchurch earthquake shows boulders from rockfalls fell much further than in earlier quakes that happened before humans arrived and changed the landscape.
Large-scale natural experiments such as oil spills, tsunamis and climate change are things you wouldn’t want to do on purpose. But that doesn’t mean they’re not scientifically useful experiments too.
Yesterday’s earthquake in central Italy has resulted in many deaths. But it is not the earthquake that claims victims but our built infrastructure. Why is this so?
There are already early warning systems for earthquakes, but advances in seismology provide hope that experts will be able to predict when new ones will occur.
Fifty years on from a groundbreaking paper, geophysicists have progressed from believing continents never moved to thinking that every movement may leave a lasting memory on our planet.