GD
Geodynamics

edited by Constanza Rodriguez Piceda

She is a postdoctoral researcher at University of Plymouth (UK). Her research interests span from the role of fault networks with complex geometries in earthquake processes to the link of the lithospheric structure with observed seismic deformation. She is co-editor-in-chief of the GD blog team.

BeGEO scientists 2025: the 3rd conference of young Earth scientists in Italy

BeGEO scientists 2025: the 3rd conference of young Earth scientists in Italy

Born at the feet of active volcanoes, a group of young Earth scientists works for connecting colleagues in Italy and around the globe. One of the main challenges faced by those approaching the academic career for the first time is creating a network of known people with whom sharing scientific knowledge and maybe lay the foundations for new collaborations. Conferences are definitely the perfect pl ...[Read More]

Silent voices, trapped minds.

Silent voices, trapped minds.

In this week’s blog post, Katherine Villavicencio (University of Chieti – Pescara) looks into the world of the mind and the mental-health issues that can result by the pressure behind a research project, such as a doctoral thesis. Here, through a personal reflexion ,she explores the main reasons that can lead candidates to suicidal thoughts, and even to the execution of them, finally a ...[Read More]

Between the Volcano and the Deep Blue Sea: Tales from Montserrat (Part 2)

Between the Volcano and the Deep Blue Sea: Tales from Montserrat (Part 2)

In 1995, the Caribbean Island of Montserrat was shaken by the beginning of one of the most significant volcanic eruptions in recent history: one that profoundly changed the natural, social and economical landscape of the country. Three decades later, Soufrière Hills Volcano and its legacy of destruction still shape the lives of Montserrat’s people. Last October, we took you on the first half of ou ...[Read More]

New Insights into Plume Buoyancy Fluxes and Dynamic Topography from Numerical Modelling

New Insights into Plume Buoyancy Fluxes and Dynamic Topography from Numerical Modelling

Figure 1. Illustration of the hotspot swell and plume buoyancy flux. White dashed line shows the original seafloor topography due to half-space cooling. Dark green line represents the surface dynamic topography caused by the dynamic uplift of the plume. One of the main surface expressions of dynamic topography are hotpot swells formed by mantle plumes. In this week’s post, Ziqi Ma, PhD candi ...[Read More]