EGU Blogs

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Geology for Global Development

Guest Blog: Women and Aid

  Nikita Kaushal is a postgraduate student in the Earth Sciences Department at the University of Oxford. Here she shares some of the key ideas about the role of women in development discussed during the 2013 OxFID conference.  Should Aid and development start with women? Gender inequality cuts across all races and communities. In development circles, women are touted as the magic cure because ...[Read More]

GeoLog

Imaggeo on Mondays: Metamorphosis

This fold is part of the metamorphic core of the Pyrenees. The shear zone is almost vertical, producing a small parasitic fold (a smaller fold within a larger one), which looks almost as if it continues into the sky. The metamorphic sediments are about 500 million years old and have been deformed several times, most recently during the alpine orogeny. The alpine orogeny was period of extensive mou ...[Read More]

Geology for Global Development

Women and Natural Hazards

“Women and children first” went the call from the deck of the titanic. And then of course Jack sacrificed his own life to save Rose, who was afloat on what admittedly looked like a raft with more than enough space for two. Chivalrous though this picture is, the reality is very different – in most disasters women seem to suffer a disproportionate number of injuries and deaths. Mos ...[Read More]

GeoLog

Presenting at the 2013 General Assembly

Oral Presentations The guidelines for oral presentations are online. The link also specifies the equipment available in each room (laptop, microphone, laser pointer, ability to hook up your own laptop, etc.). Oral presentations this year are in four 90-minute time blocks, with each talk being about 12 minutes long with 3 minutes for questions. Please be in the presentation room approximately 30 mi ...[Read More]

GeoLog

Vienna for the EGU General Assembly: arriving, sleeping and exploring the city

How to get to Vienna and what to do when you’re there – a brief, and by no means comprehensive, introduction: Getting here Vienna’s International Airport is served by many of the major European airlines. If you would like to consider overland transport (e.g train, car) there is an Information page on the EGU General Assembly 2013 website. Getting to sleep Information on accommoda ...[Read More]

GeoLog

A first-timer’s guide to the 2013 General Assembly

Will this be your first time at an EGU General Assembly? With over 11,000 participants in a massive venue, the GA can be a confusing and, at times, overwhelming place.  To help you find your way, we have compiled an introductory handbook filled with history, useful presentation pointers, and tips about Vienna and its surroundings.  Download it here!  

Geology for Global Development

Resources: Free Online Training on Responsible Mining

Impactmin offer free online training courses where you can learn more about the impact of mining. Here Peter Gyuris, the project manager of Impactmin, writes to tell us more about what the courses have to offer.   In its strictest sense, the term “Mining” refers directly to the activity of extraction of metallic or non-metallic resources from the Earth’s crust (Merriam-Webster). More commonly ...[Read More]

GeoLog

EGU 2013 General Assembly Programme now online!

The EGU General Assembly 2013 programme is available here. The scientific programme of the General Assembly 2013 includes Union Symposia, Interdivision Sessions, Educational and Outreach Symposia, as well as oral and poster sessions on disciplinary and interdisciplinary topics covering the full spectrum of the Earth, planetary and space sciences. The Keynote and Medal Lectures, Great Debate in the ...[Read More]

GeoLog

Imaggeo on Mondays: A fractured relationship – when lava meets ice

The Kuril Island Chain is formed by four active volcanoes: Golovnin, Mendeleev, Tyatya and Smirnov. Stolbchaty Cape, where the Okhotsk Sea meets the coast of Kunashir Island, is not far from Mendeleev Volcano – responsible for the many hot springs in the area. These are fed by seawater and heated as the water comes into contact with magma and hot rocks within the mantle. The picture shows an outcr ...[Read More]