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EGU25 – by the numbers
  • 6 May 2025

Thanks to the enthusiastic efforts of our members and volunteers, EGU25 was another record breaking year with an incredible 20,984 people participating in the General Assembly, both in Vienna and online!





EGU leaving Twitter/X
  • 3 March 2025

Following a vote by EGU’s volunteer Council, the Union will no longer be posting on X, formerly known as Twitter.


Latest posts from EGU blogs

Queer Quarterly: LGBTQIA+ Inclusion during fieldwork

It’s pride month and we are delighted to feature a post on queer inclusion in fieldwork written by members of EGU’s pride group. Queer Quarterly is the blog series of the EGU pride group, an LGBTQIA+ team of geoscientists engaged to uphold and improve the rights of the community at EGU. This quarterly post is based on the EGU Webinar Uneven Ground 2 on improving fieldwork accessibility for LGBTQIA+ people. Legal protections for gender and sexual minorities are in flux …


Tracking the Footprints of a Vanishing Glaciers in the Greater Caucasus

In this week’s blog, Levan Tielidze tells us about his recent glacier study from the Greater Caucasus. By combining geomorphology, remote sensing, and historical cartography, the team reconstructed nearly 200 years of glacier and climate change across one of the world’s most dynamic cryospheric frontiers. Glaciers’ transformation provides a high-resolution archive of post-Little Ice Age climate dynamics in this region where instrumental records are sparse. The Greater Caucasus and the Little Ice Age The majestic Greater Caucasus mountains, a rugged …


Highlighting: The Blatten landslide in Switzerland

In the morning of May 28, 2025, the picturesque Swiss alpine village of Blatten sat quiet and serene in the Lötschen Valley. Exceptionally quiet, in fact, as the village was evacuated on May 19th after a local Natural Hazards expert spotted a worrisome change in a local mountain looming about the village, the Kleines Nesthorn: it was collapsing faster. The Kleines Nesthorn is a 3,341-meter peak with a known instability between rock layers that has caused the mountain to shift …