Earthquakes are a key part of understanding and monitoring volcanic eruptions. Not all faults a the same am, perhaps no two are the same. And when you get one of those oceanic plates subducting between two boundary plates is effectively a subduction zone. So we've got huge earthquakes and potential fof a very large earthquake as well as sizemic hazard. Zoe so moden, what's meant by sizemic risk? What are the factors that we need to know about that? We call them megga thrust faults because there are very big sunami under water,. That also means that there are veryBig sunami as well as Sizemic Risk
Melvyn Bragg and guests discuss the study of earthquakes. A massive earthquake in 1755 devastated Lisbon, and this disaster helped inspire a new science of seismology which intensified after San Francisco in 1906 and advanced even further with the need to monitor nuclear tests around the world from 1945 onwards. While we now know so much more about what lies beneath the surface of the Earth, and how rocks move and crack, it remains impossible to predict when earthquakes will happen. Thanks to seismology, though, we have a clearer idea of where earthquakes will happen and how to make some of them less hazardous to lives and homes.
With
Rebecca Bell
Senior lecturer in Geology and Geophysics at Imperial College London
Zoe Mildon
Lecturer in Earth Sciences and Future Leaders Fellow at the University of Plymouth
And
James Hammond
Reader in Geophysics at Birkbeck, University of London
Producer: Simon Tillotson