What lies beneath – scientists discover giant trench under Antarctic Ice
Press release issued: 14 January 2014
A massive ancient subglacial trough – deeper than the Grand Canyon - has been discovered by a team of UK experts.
The research involved scientists from Newcastle University, the University of Bristol’s Glaciology Centre, the British Antarctic Survey and the universities of Edinburgh, Exeter, and York. They charted the Ellsworth Subglacial Highlands – an ancient mountain range buried beneath several kilometres of Antarctic ice - by combining data from satellites and ice-penetrating radars towed behind skidoos and on-board small aircraft.
The researchers spent three seasons investigating and mapping the region in West Antarctica, uncovering a massive subglacial valley up to 3 kilometres deep, more than 300 kilometres long and up to 25 kilometres across. In places, the floor of this valley is more than 2000 metres below sea level.
The mountain range and deep valley were carved millions of years ago by a small icefield similar to those of the present-day Antarctic Peninsula, or those of Arctic Canada and Alaska.
Professor Martin Siegert, Professor of Geosciences at the University of Bristol, said: “While the idea of West Antarctic Ice Sheet growth and decay over the past few million years has been discussed for decades, the precise location where the ice sheet may originate from in growth phases, and decay back to in periods of decay, has not been known.
“By looking at the topography beneath the ice sheet using a combination of ice-penetrating radio-echo sounding and satellite imagery, we have revealed a region which possesses classic glacial geomorphic landforms, such as u-shaped valleys and cirques, that could only have been formed by a small ice cap, similar to those seen at present in the Canadian and Russian High Arctic. The region uncovered is, therefore, the site of ice sheet genesis in West Antarctica.”
The team’s analysis has provided an unprecedented insight into the extent, thickness and behaviour of this ancient icefield, and the configuration and behaviour of the early West Antarctic Ice Sheet. The subglacial landscape shows where and how the West Antarctic Ice Sheet originated and grew. It also provides important clues about the size and shape of the ice sheet in West Antarctica in a warmer global climate.
The findings are published in the latest edition of the Geological Society of America Bulletin. The paper’s lead author Dr Neil Ross, from Newcastle University, said: “The discovery of this huge trough, and the characterisation of the surrounding mountainous landscape, was incredibly serendipitous.
“We had acquired ice penetrating radar data from both ends of this huge hidden valley, but we had no information to tell us what was in between. Satellite data was used to fill the gap, because despite being covered beneath several kilometres of ice, the valley is so vast that it can be seen from space.
“To me, this just goes to demonstrate how little we still know about the surface of our own planet. The discovery and exploration of hidden, previously-unknown landscapes is still possible and incredibly exciting, even now.”
The research was funded by the Natural Environment Research Council (NERC).
‘The Ellsworth Subglacial Highlands: Inception and retreat of the West Antarctic Ice Sheet’ by Neil Ross, Tom Jordan, Robert Bingham, Hugh Corr, Fausto Ferracciolo, Anne Le Brocq, David Rippin, Andrew Wright and Martin Siegert, is available in the Geological Society of America Bulletin.