Fault zones are far more complex than the lines we draw on geological maps. Their internal structures, mineralogical compositions, and deformation histories offer important clues to deformation mechanisms and even how earthquakes might occur. But how can we connect what we observe in the field with the microscopic processes and mechanical behaviour of faults at …[Read More]
Earth’s surface is covered by many kinds of granular materials, including sediments and soils. Below ground, grains are also widespread in unconsolidated deposits and fault zones; even polycrystalline rocks deep inside the Earth are made up of mineral grains. These materials deform under their own weight and external forces, but what forces act inside them? …[Read More]
Apart from scientific exchange and networking opportunities, conferences normally provide the chance to go places, to get out of the office, and see something new. But what happens when the conference is taking place in your home town? At your university? On your campus? Does this differ from going to other conferences or not at …[Read More]
With today’s post, I would like to temporarily leave (geo)myths behind and enter (geo)history. I was first introduced to the following historical account by Professor Francesco Brozzetti of the University of Chieti (Italy), whose extensive knowledge of the Apennines of Central Italy extends well beyond geology. Geological Origins of Monasticism This is the brief history …[Read More]
Hello there! Welcome to the TS-Blog! I’m Pauline, editor in chief. If you’re reading this, you’re probably already intrigued by our announcement and might wonder: What is it like being a blog editor? Or simply: What if the next editor of a post was… ME? Well, let me tell you more about being an editor. …[Read More]
With the EGU General Assembly 26 approaching, now is the time to review the division’s activities! Thanks to the efforts of all the conveners, and the division officers the scientific programme of our division is once again very rich and reflects the evolution of the field. Sessions The sessions are organised into nine blocks: TS1 …[Read More]
Have you ever heard of “analogue modelling”? In solid Earth science, directly observing the Earth’s interior is challenging, and the analogue modelling approach often overcomes this limitation by using alternative systems analogous to natural phenomena. By identifying fundamental mechanisms in these tractable systems, we can apply physical scaling laws to understand processes deep within the …[Read More]
The links between geomythology and science are considerable and officially began with the works of Vitaliano (EGU Blog – Geomythology. True science and/or strong communication medium ?!) and continues nowadays thanks to the Geoheritage Journal edited by Springer Nature, and evident in two proposed sessions to the EGU sessions, including one from the 2025 conference …[Read More]
The Aegadian or Egadi islands (not to be confused with the Aegean islands situated between present day Greece and Türkiye) is a small archipelago of islands around 20 km off the Western coast of Sicily. These islands are most known for their historic industries, namely for a type of rock quarried from the largest island …[Read More]
Imagine harnessing the Earth’s natural warmth to heat our homes and generate clean electricity. That is the promise of geothermal energy. It taps into the heat from beneath the Earth’s surface, providing a consistent and low-carbon power source. Geothermal energy plays a crucial role in reducing carbon emissions because it produces very little greenhouse gas …[Read More]
