Alison Parker explains how and why she ended up lecturing in International Water and Sanitation at Cranfield Water Science Institute. Over millions of years, geological forces have built the Himalayas and carved the Grand Canyon and put abundant natural resources at human beings’ disposal. However, it is obvious that in the short time that humans …[Read More]
Latest posts
The greatest story ever told, by fossils
A lot of recent(ish) posts featured on this blog have been about the evolution of flight and feathered dinosaurs. I promised to kick this habit, and write about something different, but this video by Carl Zimmer adds a really nice narrative to the story and is quite a nice little overview for anyone interested. If …[Read More]
Imaggeo on Mondays: Curl up under a peat blanket
Rannoch Moor is the largest area of unbroken (no houses, no roads) blanket bog in the United Kingdom. Blanket bogs – as their name suggests – blanket the ground in an extensive layer of peat. They form in regions where there is high rainfall and comparatively little evapotranspiration. These waterlogged conditions are found throughout much …[Read More]
Professionalism and Social Responsibility (5): Some thoughts on disseminating research
Over the past few weeks we’ve looked at a number of important factors concerned with being geologists that have a high degree of professionalism and social responsibility. These posts have included a number of practical tips on writing, preparing reports and undertaking fieldwork overseas and in different cultures. Today we explore the importance of disseminating …[Read More]
Supervisor profile – Professor Mike Kendall
Professor Mike Kendall Professor in Earth Sciences School of Earth Sciences, University of Bristol PhD (1992) “Contributions to the theory and modelling of seismic waves in anisotropic inhomogeneous media” Supervisor: Prof. C.J. Thomson 1) The Twitter challenge: Describe your PhD in 140 characters (if you can remember it) Developed theory and numerical methods to track seismic …[Read More]
Melting, microbes and methane: Are we about to face a carbon apocalypse?
Marion Ferrat takes a look under the frozen layers of Arctic permafrost and discusses how these soils may come back to haunt us. The vast plains of Siberian or Canadian permafrost are a sight to behold. Hundreds, sometimes thousands of miles of frozen soils cover these lands, a cold and barren environment. In places, however, …[Read More]
What is soil structure?
Soil structure is the result of the spatial arrangement of the solid soil particles and their associated pore space. Aggregation mainly depends on the soil composition and texture, but is also strongly influenced by other factors such as biological activity, climate, geomorphic processes or the action of fire. Structure is a typical morphological soil property, which …[Read More]
Open call for scientific sessions (EGU 2014) and more from the Soil System Sciences Division
From April 27th to May 2nd 2014 the EGU 2014 will be held in Vienna. See here more information http://www.egu2014.eu The Scientific sessions that will be held in Vienna are being uploaded now, and they will be reviewed and approved in the next council meeting of the EGU (Munich, October 10-12th 2013). The Soil System Sciences …[Read More]
Geosciences Column: Dating a bivalve
Just as the rings on a tree can be used to determine its age, the bands on a bivalve’s shell can tell us the how long it’s been around for. Warm, food-filled waters lead to greater growth in the summer and low plankton abundance (the principle food source for filter-feeding molluscs) leads to limited growth …[Read More]
Friday Photo (92): Working on Mount Etna
GPS and leveling on Mt Etna with Dr John Murray from the Open University. Credit: Rick Wall (c) Geology for Global Development 2013