A large river network lies beneath Jakobshavn Glacier.
Beneath the Jakobshavn Glacier lies a large river network carved before the formation of the Greenland Ice Sheet about 3.5 million years ago. Credit: NASA/Michael Studinger
Source: Geophysical Research Letters

Using detailed geophysical surveys of Greenland and Antarctica conducted during the past few decades, scientists can now peer below the thick glacial ice to learn more about the origin and evolution of the underlying landscape. To date, most of these studies of subglacial topography have focused on Antarctica. Now Cooper et al. have turned their attention to Greenland, where they have discovered the first evidence of an extensive network of rivers in the landscape beneath the Jakobshavn Isbræ, the island’s largest outlet glacier.

Using a digital elevation model generated from ice-penetrating radar data and corrected for the weight of the modern ice sheet, the team charted the ancient river network using two different software packages. The results of both tools reveal a dendritic network of valleys radiating inland from the Jakobshavn Glacier—a landscape that, according to the researchers, covers an area comparable in size to the Ohio River Basin and predates the formation of the ice sheet about 3.5 million years ago.

Ancient river network beneath Jakobshavn Glacier.
The ancient river network underneath Jakobshavn Isbræ basin is shown in black; a main stream of the catchment is marked by the solid red line. Bed elevation (between 300 and 1300 meters above sea level) is also shown. Credit: Cooper et al. [2016]

The team’s analysis reveals a watershed that is mostly smooth and low in elevation but also includes mountainous terrain on its eastern edge, for a total elevation range of 3382 meters. Within this basin, the team discovered very large channels up to 1400 meters deep and 12 kilometers wide—dimensions that exceed the recently reported north Greenland “megacanyon.” Their findings of low valley width-to-depth ratios, V-shaped channel cross sections, and a main channel elevation profile typical of river networks all support the conclusion that extended river incision, rather than glacial erosion, was the dominant process that formed this network.

Assuming a steady rate of incision into the hard, underlying gneiss, the researchers estimate that it would have taken about 2.3 million years to carve the observed channels, although they acknowledge that processes like glacial outbursts or increased discharge during interglacial periods could have shaped them over much shorter periods of time.

Near the basin outlet, the researchers also observed an abrupt break in slope at the confluence of three ancient channels. This knickpoint coincides with the location where the surface flow of the Jakobshavn Glacier rapidly accelerates, a finding that suggests that the underlying, preglacial landscape exerts a strong influence on the location, shape, and size of Greenland’s largest outlet glacier. (Geophysical Research Letters, doi:10.1002/2016GL069458, 2016)

—Terri Cook, Freelance Writer


Cook, T. (2016), A river network preserved beneath the Greenland ice sheet, Eos, 97, https://doi.org/10.1029/2016EO054839. Published on 28 June 2016.

Text © 2016. The authors. CC BY-NC-ND 3.0
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