GeoLog

Regular Features

Imaggeo on Mondays: Why does a Norwegian glacier look blue?

Imaggeo on Mondays: Why does a Norwegian glacier look blue?

This picture shows the outlet glacier Engabreen running down from the plateau of Svartisen in Norway. Svartisen ice cap comprises two glacier systems of which the Vestre (western) Svartisen is Norway’s second largest glacier. Located right at the polar circle, Svartisen covers a total of 369 km² of the Nordland region. These coastal mountains accumulate …[Read More]

Imaggeo on Mondays: The odd ‘living’ rocks

Imaggeo on Mondays: The odd ‘living’ rocks

Microbialites – structures which result from the interaction between microbes and sediments – have existed in the rock record since 3700 Ma ago until the present day. The presence of microbes in environments where mineral precipitation is prevalent, usually derives in the development of such chemical sedimentary structures. This can take place in marine, non-marine, …[Read More]

This calls for a celebration: GeoLog’s 1000 post!

This calls for a celebration: GeoLog’s 1000 post!

As far as blogging milestones go, today is pretty special. This is GeoLog’s 1000 post! Since the EGU’s official blog launched back in March 2010 (that’s right, there’s over 6 years of back catalogue for you to enjoy!), we’ve shared posts about research spanning almost every discipline in the Earth sciences; highlighted member’s adventures in …[Read More]

Imaggeo on Mondays: the rocks that look like Swiss cheese

Imaggeo on Mondays: the rocks that look like Swiss cheese

Over the course of centuries and millennia, the force of winds, seas, ice and rains, sculpt rock formations around the globe. From the world-famous glacier carved landscapes of Yosemite National Park, to the freeze-thawed hoodoos at Bryce National Park, through to the wind battered stone pillars of South China Karst, boundless geological formations have been …[Read More]