Earth

Spectacular Ice Age Landscapes Beneath the North Sea Revealed by 3D Seismic “MRI” Scans

Esker 3D Seismic Reflection Data Crop

Close up image of an esker (a sedimentary cast of a meltwater channel formed beneath an ice sheet), discovered within a tunnel valley using the new 3D seismic reflection data. Credit: James Kirkham

Spectacular ice age landscapes beneath the North Sea have been discovered using 3D seismic reflection technology.  Similar to MRI (magnetic resonance imaging) the images reveal in unprecedented detail huge seafloor channels – each one 10 times wider than the River Thames.

For the first time an international team of scientists can show previously undetectable landscapes that formed beneath the vast ice sheets that covered much of the UK and Western Europe thousands to millions of years ago. These ancient structures provide clues to how ice sheets react to a warming climate. The findings are published this week (September 9, 2021) in the journal Geology.

So called tunnel valleys, buried hundreds of meters beneath the seafloor in the North Sea are remnants of huge rivers that were the ‘plumbing system’ of the ancient ice sheets as they melted in response to rising air temperatures.

Lead author James Kirkham, from British Antarctic Survey (BAS) and the University of Cambridge, says:

“The origin of these channels was unresolved for over a century. This discovery will help us better understand the ongoing retreat of present-day glaciers in Antarctica and Greenland.

“In the way that we can leave footprints in the sand, glaciers leave an imprint on the land upon which they flow. Our new cutting-edge data gives us important markers of deglaciation.”

Comparing the resolution of the new high-resolution 3D seismic reflection data to previous 3D seismic data from this region. The new data revolutionises our ability to image these buried channels and their internal structures, as demonstrated by the contrast between the left and right of the image. Credit: James Kirkham, BAS

Dr. Kelly Hogan, co-author and a geophysicist at BAS, says:

“Although we have known about the huge glacial channels in the North Sea for some time, this is the first time we have imaged fine-scale landforms within them. These delicate features tell us about how water moved through the channels (beneath the ice) and even how ice simply stagnated and melted away. It is very difficult to observe what goes on underneath our large ice sheets today, particularly how moving water and sediment is affecting ice flow and we know that these are important controls on ice behavior. As a result, using these ancient channels to understand how ice will respond to changing conditions in a warming climate is extremely relevant and timely.”

A map of the North Sea showing the distribution of buried channels (tunnel valleys) that have been previously mapped using 3D seismic reflection technology. The limit of the last ice sheet to cover the UK (around 21,000 years ago) is overlain. Credit: James Kirkham

3D seismic reflection technology, which was provided by industry partners, uses sound waves to generate detailed three-dimensional representations of ancient landscapes buried deep beneath the surface of the Earth, in a similar manner to how magnetic resonance imaging (MRI) scans can image structures within the human body. The method can image features as small as a few meters beneath the surface of the Earth, even if they are buried under hundreds of meters of sediment. The exceptional detail provided by this new data reveals the imprint of how the ice interacted with the channels as they formed. By comparing these ancient ‘ice fingerprints’ to those left beneath modern glaciers, the scientists were able to reconstruct how these ancient ice sheets behaved as they receded.

Close up image of an esker (a sedimentary cast of a meltwater channel formed beneath an ice sheet), discovered within a tunnel valley using the new 3D seismic reflection data. In this image, the esker is shown in context of the high-resolution 3D seismic data which can be ‘sliced’ both vertically and horizontally to reveal ancient glacial landscapes buried beneath the seafloor of the North Sea. The reflections of the curved tunnel valley sides can be seen in the top of the image. Credit: James Kirkham

By diving into the past, this work provides a window into a future warmer world where new processes may begin to alter the plumbing system and flow behavior of the Antarctic and Greenland ice sheets.

Reference: “Tunnel valley infill and genesis revealed by high-resolution 3-D seismic data” by James D. Kirkham, Kelly A. Hogan, Robert D. Larter, Ed Self, Ken Games, Mads Huuse, Margaret A. Stewart, Dag Ottesen, Neil S. Arnold and Julian A. Dowdeswell, 8 September 2021, Geology.
DOI: 10.1130/G49048.1

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  • "3D seismic reflection technology, ..., uses sound waves to generate detailed three-dimensional representations of ancient landscapes buried deep beneath the surface of the Earth, in a similar manner to how magnetic resonance imaging (MRI) scans can image structures within the human body."

    Similar in what ways? MRI doesn't use sound waves. Instead of dumbing it down so much that it misinforms, why not take the time to just explain how 3D seismic reflection imaging works, and educate the laymen reading the article?

    https://en.wikipedia.org/wiki/Magnetic_resonance_imaging

  • Having worked in a glaciated mountainous region where glaciers had been melting since the 1890s I would expect that much of the glacial erosion is done by melt-water carrying rocks that have dropped onto the glacier by landslides and which have become incorporated into the glacier and then into its meltwater sinkholes before being washed out as nicell rounded pebbles at the snout of the glacier. Ice-plucking of bedrock no doubt occurs but the maximum erosion would surely be akin to sand-blastng by water-borne debris below and along the side of the glacier. In turn we would see oversteepening of valley sides and additional consequent slumping of large blocks of the mountains together with destabilisation by ice-melt of the former frozen fractured rocks of the valley sides.This would dump additional debris on the glacier to continue the erosive processes in due course. There is a feed-back mechanism involved; the more the glacier melts, the more the landsliding and the more the basal erosion.

  • You had to check a box confirming you are not a spammer. Since you lied, why should anyone believe your claims about easy money?

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British Antarctic Survey

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