“There is no such thing as ‘just’ ice.” Not to a glaciologist anyway.
Professor Doug Benn is recounting to us his reply to a reviewer who questioned his use of the term ‘refrozen water ice’. While this may sound superfluous, the many variations in density, temperature, content, layering, and colour of glacier ice can tell us a lot about its history, and potentially, about it’s future.
At the beginning of August, I was fortunate enough to take part in the International Glaciology Summer School, in beautiful Alaska. The school is run every two years, directed by Regine Hock of the University of Alaska Fairbanks, and brings together students and instructors from all over the world. Based in the Wrangell mountains, in the old mining village of McCarthy, the school provides an opportunity to learn from experts in a range of fields within glaciology, and perhaps more importantly, provides a platform to engage with and get to know others embarking on research in the science. The 10 days of the course were some of the most enjoyable of my academic career, and I left inspired by the enthusiasm and curiosity of my peers.
Below are images from some of the activities that took place outside of the classroom (click on images to enlarge).