Glen More, on the Isle of Mull, Scotland, is a classic locality for studying glacial landforms and sediments. Here, two prominent ice-transported boulders stand guard at the head of the valley, left behind after the Loch Lomond Readvance (Younger Dryas stade), the final pulse of Quaternary glaciation in Scotland. Behind them in the characteristic U-shaped valley, hummocky morraines are littered wi ...[Read More]
GeoPolicy: Communicate Geoscience? Let’s do it!
This month’s GeoPolicy Column was written by Alexander Roesner, a researcher at MARUM (the Center for Marine Environmental Sciences) and the winner of the EGU’s 2019 ECS Policy Competition, which provides the winner with funding to attend the EGU’s science-policy event, Shaping EU Missions in Brussels. Roesner outlines his motivation for applying for the competition and reflects on his experience. ...[Read More]
Imaggeo on Mondays: Great sand dunes and beyond
Driving eastwards through the San Luis Valley in south central Colorado, United States, the Great Sand Dunes emerge at the foot of the Sangre de Cristo Range in the northeast of the region’s upland plain. The origin story of these great dunes begins during a time of glacial melt, five to three million years ago, when the rivers of the surrounding mountains filled the basin with water and sediments ...[Read More]
Imaggeo on Mondays: Civita di Bagnoregio – the dying town
On top of a steep cliff standing out from the surrounding countryside, lies the small town of Civita di Bagnoregio, one of the most famous villages of Italy. It is often called the dying town, although more recently people have started to refer to it as fighting to live. What this little town is fighting against is the threat of erosion, as its walls are slowly crumbling down. Located in central I ...[Read More]