Smoky Summer It has been a difficult summer in Alberta, with smoke from forest fires in British Columbia blanketing much of the southern part of the Province. However, this has not stopped me getting out into the field on a variety of projects and hikes, including a virtual field trip looking at the Cardium Formation …[Read More]
Division blogs
Curious case of convex upwards topography in accretionary wedges
Accretionary prisms are wedge-shaped bodies of crustal rocks that are commonly known to have formed by accommodating the component of convergence along subduction margins. These prisms, primarily wedge shaped with lateral variations in topographic height from hinterland to foreland are commonly characterised by a gentle and uniform slope towards the frontal margin (for instance, the …[Read More]
The road to successful scientific writing for early-career scientists
The world of research is highly competitive, and early career scientists face many challenges while trying to carve out a successful career path. Writing scientific articles is one of those challenges. Prof. Paolo Tarolli (University of Padova) shared his personal experience on “How to write a scientific article” with 130 attendees last 7th September, during …[Read More]
TS Must-Read – England and Molnar (1990) Surface uplift, uplift of rocks, and exhumation of rocks
With this paper, England and Molnar (1990) shed light on the recurrent confusion in the uses of terms ‘uplift’ and ‘exhumation’. The main focus is to clarify the difference between surface uplift, uplift of rocks, and exhumation by explaining the differences and the relations between these processes (Fig. 1). The manuscript also illustrates how other …[Read More]
Will the Arctic be ice free earlier than previously thought?
There is no doubt that the Arctic is currently losing its sea ice as our climate is warming. And this process will carry on as temperatures continue climbing. But the rate at which sea ice will melt in the future and the exact date when the Arctic will be free of sea ice is not …[Read More]
The Sassy Scientist – Postdoc Purgatory
Postdoc appointments: the forgotten terrace of Purgatory. Where researchers are sentenced to linger till either a position opens in the Heaven of permanent contracts, or they realise that, after all, they are not interested anymore. This terrace is composed of different levels of various length. Nobody knows how many levels there are and how long …[Read More]
Getting to the core of The Core
Imagine my surprise when I found out that one of the regular attendees of our virtual institute coffee in Leeds actually worked on the movie ‘The Core’. Yes, you read that correctly: The Core, maybe the best bad science movie out there! (Although Menno had some great other suggestions last week!) So, in between many …[Read More]
TS Must-Read – Dahlen (1990) Critical Taper Model Of Fold-and-thrust Belts And Accretionary Wedges
Dahlen 1990‘s paper presents a synthesis of all theoretical work on accretionary wedges that had begun more than a decade earlier, with the fold and thrust belts research of Elliott (1976), Chapple (1978), and model by Davis et al., (1983). Dahlen expanded previous views with a more sophisticated treatment of pore-fluid pressure using volume-averaged Stokes-equations …[Read More]
Mapping sea ice from space
Reduced and thinner sea ice makes Arctic waters increasingly appealing for shipping, fishing, tourism, and mineral exploration. However, with increased accessibility and more dynamic ice conditions comes a greater risk for ship crews to encounter sea ice and icebergs outside of their usual seasonal limits. To help them navigate, timely and reliable sea ice information …[Read More]
The Sassy Scientist – Comment – Reply – Comment – Reply – …
Diane is on top of her research. Not only that, her education is unparalleled and with this background she is therefore in a perfect position to adjudicate the works of others: A scientist I know published a paper drawing the wrong conclusions from their own research. How should I let them know? Dear Diane, As …[Read More]