Stratigraphy, Sedimentology and Palaeontology

Imaggeo on Mondays: Tones of sand

Laura Roberts-Artal January 2, 2017

Tones of sand Credit: Marc Girons Lopez (distributed via imaggeo.egu.eu

With rocks dating as far back as the Precambrian, mountain building events, violent volcanic eruptions and being covered, on and off, by shallow seas, Death Valley’s geological history is long and complex. Back in the Cenozoic (65 to 30 million years ago), following a turbulent period which saw the eruption of volcanoes (which in time would form the Sierra Nevada of California) and regional uplift ...[Read More]

The best of Imaggeo in 2016: in pictures

Laura Roberts-Artal December 26, 2016

The best images of 2016, from imaggeo, as chosen by our readers and followers.

Imaggeo, our open access image repository, is packed with beautiful images showcasing the best of the Earth, space and planetary sciences. Throughout the year we use the photographs submitted to the repository to illustrate our social media and blog posts. For the past few years we’ve celebrated the end of the year by rounding-up some of the best Imaggeo images. But it’s no easy task to pick which ...[Read More]

GeoEd: A round-up of (geo)educational board games

Laura Roberts-Artal November 23, 2016

Playing the Wiapuna board game in the final class. Credit: T. Ewen and J. Seibert, 2016.

With the rise of electronic games – those played on computers, consoles and even on mobile phones – you’d be forgiven for thinking the humble board game would be slowly making its way into the history books. Nothing could be further from the truth! Sales of board games are on the up, as are cafes where you can gather to play table-top games of your choice, and board game meet ups: regular gaming g ...[Read More]

Imaggeo on Mondays: The odd ‘living’ rocks

Laura Roberts-Artal October 17, 2016

Huepac stromatolites . Credit: Hugo Beraldi (distributed via imaggeo.egu.eu)

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, and subterranean environm ...[Read More]