San Francisco has been a natural gathering place for people across the millennia. It is not a coincidence that this city, situated at the entrance to the largest estuary on the U.S. West Coast, owes its dramatic setting to active geology on the North American plate margin. The first people of the San Francisco Peninsula, the Ramaytush Ohlone, cared for the land here for thousands of years before E ...[Read More]
Mind your head: Overcoming Anxiety
This Mind Your Head blog post is a follow-up from Jean Holloway’s talk during the online short course on mental health that aired during the last EGU General Assembly, where she discussed overcoming anxiety. Anxiety is excessive worry or fear, and is a normal part of life, until it becomes frequent or debilitating. This post is written by someone with lived experience as an academic who struggled ...[Read More]
Zürich: surrounded by a geologist’s playground
Zürich, with its lake stretching towards the foot of the Swiss Alps in the South, is currently a charming city full of watersides, lively bars, students and bankers. In Switzerland, you’ll find a wide variety of landscapes and geological features over a relatively small area – from the Alpine mountain range in the South to the low-lying plateau and the Jura Mountains in the North. Located in close ...[Read More]
Sendai, living on the edge!
Sendai and its people live on the edge. The city and its citizens learned to live over a subduction zone. Sendai has survived 500 years of hazards; it is a resilient and industrious city. People know disaster will strike again, but also that they will rise up when it does. Japan, ‘the sunrise country’, would be much better named ‘the land of sinking tectonic plates’. Above the point where the Paci ...[Read More]
Trieste, where the word Karst originates
The city of Trieste lies in north-eastern Italy along the border with Slovenia. It is positioned at the corner point between the Romance, Germanic and Slavic worlds and serves as an important seaport in the region. It is fascinating for both its history and geology. My relationship with Italy’s town of Science, as Trieste is often referred to, started about a year ago. I got the opportunity to st ...[Read More]
Minds over Methods: Dating deformation with U-Pb carbonate geochronology
For this edition of Minds over Methods, we have invited Nick Roberts, a research scientist at the British Geological Survey, working within the Geochronology and Tracers Facility (GTF) running a LA-ICP-MS laboratory. Nick has a background in ‘hard-rock’ geology, incorporating geochemistry, geochronology, and magmatic and metamorphic petrology across a wide range of tectonic settings, and is now in ...[Read More]
Minds over Methods: Virtual Microscopy for Geosciences
The next “Minds over Methods” blogpost is a group effort of Liene Spruženiece (left) – postdoctoral researcher at RWTH Aachen and her colleagues Joyce Schmatz, Simon Virgo and Janos L. Urai. The Virtual Microscope is a collaborative project between RWTH Aachen University and Fraunhofer Institute for Applied Information Technology (Schmatz et al., 2010; Virgo et al., 2016). In the ...[Read More]
From Mountains to Modernists: the geological foundations and inspirations of Barcelona
Barcelona is a vibrant city on the Mediterranean coast, nested snugly between the sea and the Collserola Ridge of the Catalan Coastal ranges. The story of Barcelona starts around 2000 years ago as an Iberian settlement, owing to its strategic location on the coastal route connecting Iberia and Europe. The combination of easily defendable ground and the fertile soils of the Besos and Llobregat delt ...[Read More]
Minds over Methods: The faults of a rift
Do ancient structures control present earthquakes in the East African Rift? Åke Fagereng, Reader in Structural Geology, School of Earth and Ocean Sciences, Cardiff University For this edition of Minds over Methods, we have invited Åke Fagereng, reader in Structural Geology at the School of Earth and Ocean Sciences, Cardiff University. Åke writes about faults in the Malawi rift, and the seismic ha ...[Read More]
Features from the field: Boudinage
The Features from the Field series is back! In our previous posts, we have shown how rocks can deform during ductile deformation, producing folds. Folds very commonly develop in rocks when rock layers are shortened by tectonic forces in a specific direction. On the other hand, when layers are extended, we develop boudins. Boudins – the term comes from the French word for ‘sausage’ – are frag ...[Read More]