Self-reflection

Changing mid-degree: How did this Travelin’ Geo get here?

Leiaka Welcome and edited by Kiran Chotalia January 12, 2022

Figure 1: Being used for scale by a colleague to detail extensive cross bedding in southern Utah (Triassic outcrop).

It can be tough realising you’re not on the path you want to be on. This week, we have Leiaka Welcome from the Colorado School of Mines showing us how a change of heart led her to start her PhD journey. Currently on social media (Instagram Reel, TikTok), there is a video trend where users are editing a video of themselves in a scenario with an audio sound where you can hear a classic record scratc ...[Read More]

Carbon in the cloud

Eoghan Totten and edited by Lucía Pérez-Díaz February 10, 2021

If I asked you about what your carbon footprint is, your mind might jump to the food choices you make when at the supermarket, or how many conferences you fly to when you could get a train (well, not now, but you know, back in ye olden days). In this week’s post, Eoghan Totten, a PhD student at the University of Oxford, discusses the potential “hidden” impacts on your contributio ...[Read More]

The Sassy Scientist – To Beer Or Not To Beer?

The Sassy Scientist November 27, 2020

Theeerre ish noffink quite so dangerereroush as ashkink a seeeriouss question of scieeence at 18h30 on a Friday. Rudi inshtead ashks the not-at-all, definitely-not, who-me, ashking-for-a-friend queshtion: Can I get drunk at Friday Beers? Dear Rudi, Your question has more answers than asking a conference of geodynamicists what’s the best wine? With movement and beer restrictions in place, the ...[Read More]

What can we learn from geodynamic failure?

Moh Gouiza and edited by Lucía Pérez-Díaz October 28, 2020

AllMyFault by L. Perez Diaz is licensed under a Creative Commons Attribution-NoDerivatives 4.0 International License.

In this week’s post, Mohamed Gouiza discusses the challenges of living under constant stress, paralysed by the possibility of failure and self-perceived inevitability of impending breakup. Continental rifting, of course! Oh… did you think I was talking about life as a researcher? Under tensile stress, the lithosphere stretches, the asthenosphere rises, the crust fails, and rifts form. During this ...[Read More]