Detail of a photo: Large angular boulder beside a shallow pebbly stream in a grassy mountain valley, below steep forested slopes and rocky peaks under a dramatic blue sky, in heavily processed colours.
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GD

Join in our Mag-netZ !

Join in our Mag-netZ !

For better or for worse, online seminars have stealthily become part of our routine. This week, Daniele Thallner from the University of Florida, “attracts” our attention to a seminar series on geomagnetism and geodynamo modeling — Mag-netZ! The 2022 season of the MagNetZ seminar series is live! The MagNetZ (Magnetic NetworkZ) online seminar series was …[Read More]

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The Sassy Scientist – Seminar Yoga

The Sassy Scientist – Seminar Yoga

Chairing conference sessions, organising social events, writing on the EGU blog site: extra-curricular activities can help rounding up our scientific and academic identity. But let’s face it, they take up time and they can be stressful. Seynabou has been (surely very democratically, as it always happens) appointed as group meetings organiser but finds herself in …[Read More]

NH

Life with dust: its impacts and how to catch it

Life with dust: its impacts and how to catch it

In today’s interview, we have the pleasure to meet Dr Slobodan Nickovic, who won the prestigious 2022 Plinius Medal. Slobodan is a research consultant at the Republic Hydrometeorological Service of Serbia, and at the Institute of Physics in Belgrade, Serbia. Throughout his career, he worked for national and international educational, scientific, and operational institutions including …[Read More]

TS

TS Must-Read – Cowie (1998) A healing-reloading feedback control on the growth rate of seismogenic faults

TS Must-Read – Cowie (1998) A healing-reloading feedback control on the growth rate of seismogenic faults

This study provides a simple numerical model of fault rupture that describes the development of fault systems from the initial nucleation of numerous small faults to the localisation of deformation into few major faults. The model presented is based on two main considerations: first, earthquakes cause stress changes that can either advance or delay failure …[Read More]