Regular Features

Imaggeo on Mondays: Mirror Image

Laura Roberts-Artal April 6, 2015

Water reflection in Svalbard. Credit: Fabien Darrouzet (distributed via imaggeo.egu.eu)

This week’s Imaggeo on Mondays image is brought to you by Fabien Darrouzet, who visited the icy landscapes of Svalbard back in 2012. Whilst the aim of his trip was not to better understand the geology of the landscapes, his eyes were very much focused on goings on up, up in the sky, it didn’t stop him taking this still of the snow covered peaks. This picture was taken in Svalbard (78° lat.) in Jun ...[Read More]

Imaggeo on Mondays: Drumlins Clew Bay

Laura Roberts-Artal March 30, 2015

Drumlins Clew Bay Credit: Pete Coxon (distributed via imaggeo.egu.eu)

During ice ages landscapes are sculpted by the power of advancing glaciers. From rock scratches, to changing mountains and the formation of corries, cirques and aretes, through to the formation of valleys and fjords, the effects of past glaciations are evident across the northern hemisphere landscape. Perhaps not so familiar, drumlin fields are also vestiges of the erosive power of ancient ice she ...[Read More]

GeoEd: Lessons from the EGU 2014 GIFT Workshop

Laura Roberts-Artal March 27, 2015

Today’s GeoEd post is brought to you by Susan Tate, an 8th grade teacher from Michigan in the USA. Susan attended the GIFT workshop held during the General Assembly last year. The GIFT programme offers primary school to high school teachers the opportunity to upgrade their knowledge in geophysical themes and to shorten the time between new discoveries and textbook information. After three d ...[Read More]

Imaggeo on Mondays: Escullos

Laura Roberts-Artal March 23, 2015

Escullos. Credit: Alicia Morugán (distributed via imaggeo.egu.eu)

This picture shows a Quaternary aeolianite fossil dune at the Escullos beach, in the Nature Reserve of Cabo de Gata (Almeria, Spain). Originally a soft accumulation of sand grains, shaped by the wind into large mounds and ridges, the dunes eventually turn into rock. As the sediments compact under their own pressure and expel any moisture and fluids retained within them, they become lithified and b ...[Read More]