GMPV
Geochemistry, Mineralogy, Petrology & Volcanology

EGU

EGU GMPV ECS Campfires – Special Edition Thursday 16th November 4pm CET

EGU GMPV ECS Campfires – Special Edition Thursday 16th November 4pm CET

After a pause, the Geochemistry, Mineralogy, Petrology and Volcanology division’s early career scientists talks (EGU campfires) are back! The first session in 2023 will be a special relaunch event. It will be held on Thursday 16th November at 4pm CET on Zoom. For this special edition, our speaker is Xin Zhong (PostDoc @ Freie Universität Berlin, Germany) on “the effect of aqueous fluid on viscous ...[Read More]

Call for new blog editors!

Call for new blog editors!

The Geochemistry, Mineralogy, Petrology and Volcanology division of the European Geosciences Union is looking for two new blog writers that can join our team! We are a group of 16 early career scientists, coming from all over the world, and with different backgrounds. If you wanna know more about our team, and what we do during the year, have a look here! We are looking for individuals that like s ...[Read More]

Meet the GMPV Early Career Scientists group!

Meet the GMPV Early Career Scientists group!

2023 has been a year of big changes in the GMPV Division, with our new President Holly J. Stein, and in the GMPV Early Career Scientists (ECS) Committee, with new ECS Representative, Blog in Chief Editor and Chief organizer of the Campfires! First of all, we would like to thank Giulia Consuma for her amazing work as ECS Representative of our division for the years GA/2022-2023 and as Campires orga ...[Read More]

The role of Geothermal Energy in the energetic and environmental challenge.

The role of Geothermal Energy in the energetic and environmental challenge.

How does a Geothermal system work?  Heat is a form of energy and, strictly speaking, geothermal energy is heat from inside the Earth. The large amount of thermal energy enclosed below the earth’s surface derives in part from its primordial formation process and in part originates from the decay of radioactive isotopes present mainly in the earth’s crust and, secondarily, in the mantle. ...[Read More]