GMPV
Geochemistry, Mineralogy, Petrology & Volcanology

Geology

Geological TrIPS: The amazing fragments of oceanic crust treasured on the Greek island of Syros

Geological TrIPS: The amazing fragments of oceanic crust treasured on the Greek island of Syros

Geologists are often fascinated by the processes (and their products) taking place at the sea. Perhaps the fact that we do not have easy access to most of these processes is what puzzles us as geoscientists. Subduction can be considered as one of these “mysterious” processes for which several mechanisms remain to be better understood. Fortunately, subduction zones can be studied through their anci ...[Read More]

A Geologist’s Dream Vacation: Exploring Europe’s Volcanic Wonders!

A Geologist’s Dream Vacation: Exploring Europe’s Volcanic Wonders!

Summer time can be stressful – you have plenty of things to do at work but at the same time you’re thinking about your next vacation all the time. This is at least how I was feeling, combined with some curiosity, I asked chatGPT to write a blog post about vacation destinations for geologist around volcanoes in Europe – here are the results, I hope you get inspired:  Calling all g ...[Read More]

Elemental etymology – what’s in a name?

Photo of a medieval medical manuscript translated from Arabic in the 2nd half of the 13th Century.

Like many scientists in the GMPV sphere, I work a lot with geochemistry – using chemical elements and their differing behaviours, abundances or isotopes as tools to understand Earth processes. While staring at the periodic table, something that’s always niggled at me is where the names of these come from: why is the stuff we breath called oxygen and the sand on the beach made of silicon? Even more ...[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]