The deadline for submitting nominations is arriving soon. So it is the perfect time for EGU Geodynamics President Jeroen van Hunen to explain what awards there are and how easy it is to nominate you colleague for it! This is my first-ever EGU GD blog (in fact, this is the first time I am writing a blog at all). I feel like stepping into a new world. The topic of this blog is EGU medals and awards. ...[Read More]
Whole solid-Earth numerical simulation: Towards an understanding of mantle-core interactive dynamics
Due to huge difference between the time scale of the mantle convection and the outer core convection, they are modelled separately. In this week’s News and Views, Masaki Yoshida from the Volcanoes and Earth’s Interior Research Center, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japan, put forward the recent development on the modeling of the whole solid-Earth. The E ...[Read More]
Expand your toolbox: Three new programming languages to try out
Geodynamists usually do at least a bit of programming, but in many cases a lot of programming, although that might just be my academic bubble. Most of that programming is done in programming languages that have been around at least since the 80’s (Fortran, C and C++) or early 90’s (Python). These programming languages have of course evolved considerably over time, but new languages keep popping up ...[Read More]
Finding stillness in chaos: The emergence of stable cratons in a hectic young Earth

Today we know the Earth as a tectonically busy planet, shaped by mantle convection and plate tectonics. But this is nothing compared to the earlier phases of planetary evolution. This week, Fabio Capitanio (ARC Future Fellow and Associate Professor at the School of Earth, Atmosphere and Environment at Monash University, Australia) takes us on a modelling tour back to a time when the Earth’s tecton ...[Read More]