Imaggeo

Imaggeo on Mondays: Breath from the underground

Laura Roberts-Artal June 26, 2017

Breath of the underground . Credit: Néstor Campos (distributed via imaggeo.egu.eu).

The heat seeping from the geothermal area which is part of the Krafla volcanic system in Iceland, ‘powers’ the steaming vent at Hverir (Hverarönd). The area is well known for its mud pots and sulphuric gas fumaroles, complete with pungent eggy smell. Some of the vents are in fact boreholes drilled in the 50’s for sulphur exploration which have been turned into fumaroles, the steam is a resul ...[Read More]

Imaggeo on Mondays: Erebus Ice Tongue Cave

Laura Roberts-Artal June 12, 2017

Erbus Ice Tongue Cave . Credit: Hinrich Schaefer (distributed via imaggeo.egu.eu).

The interior of this ice cave at the Erebus glacier tongue is cathedral-like. Imagine standing in the cold interior, icy blue stalactites dangling from the cave roof; the sense of awe is overwhelming. Mt. Erbus is the world’s southernmost active volcano on Ross Island, in Antarctica. Winding its way down its lower slopes is Erebus glacier. Projecting out from the coast, a jagged and thin tongue ma ...[Read More]

GeoSciences Column: Can seismic signals help understand landslides and rockfalls?

Laura Roberts-Artal June 9, 2017

Landslide Gschliefgraben . Credit: Robert Supper (distributed via imaggeo.egu.eu).

From the top of a small gully in the French Alps, a 472 kg block is launched into the chasm. Every detail of it’s trajectory down the slope is scrutinised by two cameras and a network of seismometers. They zealously record every bounce, scrape and tumble – precious data in the quest to better understand landslides. What makes landslides tick? In 2016, fatalities caused by landslides tipped 2 ...[Read More]

Imaggeo on Mondays: A lava layer cake

Laura Roberts-Artal May 29, 2017

A lava layer cake flowing . Credit: Timothée Duguet (distributed via imaggeo.egu.eu)

Brekkuselslækur, a small river, carves its way across Iceland’s ancient volcanic landscape. At Hengifoss, Iceland’s third-highest waterfall, it tumbles fiercely down thick, dark layers of lavas erupted from volcanoes some 18 to 2.58 million years ago, during a period of geological time known as the Tertiary. Eruptions are rarely continuous; during hiatuses in the extrusion of lavas, ash is able to ...[Read More]