Last year we introduced the ASPECT hackaton on this geodynamics blog. It was the first hackathon which went virtual which brought a whole set of new challenges. This year was the 8th version of the yearly hackathon, and it was still virtual (unfortunately). Fortunately lessons where learned from the previous virutal hackathon and generally from …[Read More]
Latest posts
Stratigraphy, Sedimentology and Palaeontology
An online learning platform for cyclostratigraphy – www.cyclostratigraphy.org
Cyclostratigraphers aim to read and understand the effect of climate-driven orbital changes in the geological record through time. In doing so, they start from an important prerequisite: An imprint of insolation variations caused by Earth’s orbital eccentricity, obliquity and/or precession (Milankovitch forcing) can be preserved in the geological rock record. The new www.cyclostratigraphy.org website is …[Read More]
Climate: Past, Present & Future
An online learning platform for cyclostratigraphy – www.cyclostratigraphy.org
Cyclostratigraphers aim to read and understand the effect of climate-driven orbital changes in the geological record through time. In doing so, they start from an important prerequisite: An imprint of insolation variations caused by Earth’s orbital eccentricity, obliquity and/or precession (Milankovitch forcing) can be preserved in the geological rock record. The new www.cyclostratigraphy.org website is …[Read More]
GeoLog
Imaggeo On Monday: Geodesy on Zugspitze
The Zugspitze Geodynamic Observatory Germany (ZUGOG) has been setup on the summit of mountain Zugspitze at an altitude of almost 3000 m during 2018 with the main scientific objective being a better understanding of seasonal and long-term mass redistributions in the European Alps. This knowledge is very important (e.g. with regard to water storage and …[Read More]
Geodesy
Notes from a hybrid conference
With the COVID pandemic still ongoing, many conferences have been taking place online or have opted for a hybrid format, with combined on-site and online program parts. To many of us this still a rather new experience, so we decided to share some of the impressions we gathered in the hybrid meetings we attended so …[Read More]
GeoLog
GeoRoundup: the highlights of EGU Journals published during July!
Each month we feature specific Divisions of EGU and during the monthly GeoRoundup we will be putting the journals that publish science from those Divisions at the top of the Highlights roundup. For July, the Divisions we are featuring are: Natural Hazards (NH) and Geomorphology (GM). They are served by the journals: Geoscientific Model Development (GMD), …[Read More]
Geodynamics
The Sassy Scientist – The Virtual Welcome Drink
We live in crazy times! Remember the times when we could just hang out with people without fear of being infected by a life-threatening desease? Me neither. Fasim asks a question that must be keeping a lot of us up at night: First day on new job in quarantine…what do I do? Dear Fasim, First …[Read More]
GeoLog
GeoPolicy: A Climate and Ecological Emergency: Can a pandemic help save us…?
The EGU’s #vEGU21 streamed a wide variety of virtual sessions from Short Courses to Union Symposia. While most #vEGU21 sessions had a specific scientific focus, a few highlighted topics that were of interest to geoscientists across multiple disciplines. The Union Symposia 3: “A Climate and Ecological Emergency: Can a pandemic help save us…?” was one …[Read More]
Geodynamics
Plate tectonics from a perspective of continental crustal growth
Understanding the plate tectonics initiation can give us incredible opportunity to guess the physical state of the early Earth. This week, Hee Choi, a Ph.D. candidate, takes us on a journey on initiation of plate tectonics and how continental crustal growth is related to it. Our planet Earth is the only place where plate tectonics …[Read More]
Geochemistry, Mineralogy, Petrology & Volcanology
Drilling in the deep: Project Mohole and the underground space race
The mantle makes up the bulk of Earth, extending from near the surface to the edge of the core 2900 km down. It constitutes 84% of Earth’s volume and has roughly 6 times the mass of Mars! Despite its impressive bulk, the mantle is almost everywhere covered by several km of crust. As a result …[Read More]