Tectonics and Structural Geology

Imaggeo on Mondays: The road to nowhere – natural hazards in the Peloponnese

Laura Roberts-Artal September 19, 2016

Find a new way . Credit: Romain Hemelsdael (distributed via imaggeo.egu.eu)

The Gulf of Corinth, in southern Greece, separates the Peloponnese peninsula from the continental mainland. The structural geology of the region is complex, largely defined by the subduction of the African Plate below the Eurasian Plate (a little to the south). The Gulf itself is an active extensional marine basin, i.e., one that is pulling open and where sediments accumulate. Sedimentary basins r ...[Read More]

What is in your field rucksack? Camping in Iceland

Laura Roberts-Artal September 16, 2016

Inspired by a post on Lifehacker on what your average geologist carries in their rucksack/backpack, we’ve put together a few blog posts showcasing what a range of our EGU members carry in their bags whilst in the field! Beautiful, eyrie, the land where fire meets ice: Iceland. An Earth scientist’ dream, complete with lava, volcanoes, earthquakes, impossible landscapes, ice, snow, the ocean…Iceland ...[Read More]

Imaggeo on Mondays: A Bubbling Cauldron

Jamie Farquharson August 1, 2016

Bubbling Cauldron . Credit: Jamie Farquharson (distributed via imaggeo.egu.eu)

Despite being a natural hazard which requires careful management, there is no doubt that there is something awe inspiring about volcanic eruptions. To see an erupting volcano up close, even fly through the plume, is the thing of dreams. That’s exactly what Jamie Farquharson, a researcher at Université de Strasbourg (France) managed to do during the eruption of the Icelandic volcano Bárðarbunga. R ...[Read More]

Imaggeo on Mondays: an impressive testimony to the collision between Africa and Europe

Angelika Jung-Hüttl July 18, 2016

Dent de Morcles, The Waadtland Alps, Switzerland . Credit: Bernhard Edmaier (distributed via imaggeo.egu.eu)

The huge fold in the flank of the 2969 m high Dent de Morcles (in Waadtland Alps, Switzerland) is an impressive testimony to the collision between Africa and Europe (which began some 65 million years ago). The layers, originally deposited on the sea floor in a horizontal position, were compressed and shifted. The darker parts developed during the Tertiary period (66 million years ago). They are yo ...[Read More]