Cookies

We use cookies to ensure that we give you the best experience on our website. You can change your cookie settings at any time. Otherwise, we'll assume you're OK to continue.

Durham University

Department of Geography

Departmental Research Projects

Testing the Instability Mechanism for Subglacial Bedform Production

A research project of the Department of Geography.

Background

When ice sheets flow across the landscape they often produce particular landforms, the best known of which are drumlins. These are elongate streamlined hills, kilometres in length and tens of metres in height. Mega-scale glacial lineations (MSGL) are similar to drumlins but exist at huge scales (up to 100km in length). They record the ice flow direction at the time at which they were formed, and our contention is that if we know how they formed, then we would learn much more about how ice sheets flow. Understanding the formation of subglacial bedforms, such as drumlins and MSGL has suddenly become very important because society is concerned about how the ice sheets in Antarctica might respond to global warming.

The approach that we take in this project, funded by the Natural Environment Research Council, is based on a simple idea drawn from how nature works to produce other (non-glacial) types of patterns. A classic example is wave-like patterns in clouds. Such repetitive patterns are known to form by instability mechanisms. Instability is said to occur in a system when very small irregularities (say in air flow in a cloud) spontaneously grow and often produce regular patterns. We view subglacial bedforms as repetitive patterns and propose that some form of instability produced them.

By mathematical analysis and computer-modelling we have already established that the interacting flow of ice and the underlying sediment can produce instabilities. But this is not enough to convince us that it is the right answer. We now need to establish if instabilities grow to produce landforms, such as the drumlins, which we can observe in real life. If for example the instability only produces landforms 5mm in size or 1000km in size, or of the wrong shape, then we know we have got it wrong. As such, we will map and measure drumlins and mega-scale lineations (around 60,000 examples) that exist in Canada, UK, and Ireland and on the seafloor around Antarctica to see what their size and characteristics are. This cannot be achieved by fieldwork and so we will use satellite images and geophysics. The data will be used to test the modelling. If the model turns out to be correct then the results become critical for understanding ice streams and will help predict their future behaviour. Also, we anticipate that whole assemblages of landforms beneath the Antarctic Ice Sheet will soon be found. Our results will provide a sound physical basis for interpreting what they tell us.

Classically shaped drumlins of Ribblesdale, Yorkshire Dales, England formed by ice flow from north to south (from Clark et al., 2009).

Selected Publications

Stokes, C.R., Spagnolo, M. and Clark, C.D. (2011) The composition and internal structure of drumlins: complexity, commonality, and implications for a unifying theory of their formation. Earth-Science Reviews, 107, 398-422.

Spagnolo, M., Clark, C.D., Hughes, A.L.C., Dunlop, P. and Stokes, C.R. (2010) The planar shape of drumlins. Sedimentary Geology, 232, 119-129.

Clark, C.D., Hughes, A.L.C., Greenwood, S.L., Spagnolo, M., & Ng, F.S.L. (2009). Size and shape characteristics of drumlins, derived from a large sample, and associated scaling laws. Quaternary Science Reviews., 28, 677-692.

Fowler, A.C. (2010) The formation of subglacial streams and mega-scale glacial lineations. Proceedings of Royal Society, A, Mathematical, Physical and Engineering Sciences, 466 (2123), 3181-3201.

Fowler, A.C. (2009) Instability modelling of drumlin formation incorporating lee-side cavity growth. Proceedings of Royal Society, A, Mathematical, Physical and Engineering Sciences, 465, 2681 - 2702.

King, E.C., Hindmarsh, R.C.A. and Stokes, C.R. (2009). Formation of mega-scale glacial lineations observed beneath a West Antarctic ice stream. Nature Geoscience, 2, 585-588.

Hindmarsh, R.C.A. & Stokes, C.R. (2008). Formation mechanisms for ice-stream shear margin moraines. Earth Surface Processes and Landforms, 33, 610-626.

Dunlop, P., Clark, C.D., and Hindmarsh, R.C.A. (2008). Bed Ribbing Instability Explanation: Testing a numerical model of ribbed moraine formation arising from coupled flow of ice and subglacial sediment. Journal of Geophysical Research, 113 (F3), F03005.

Fowler, A.C. (2010) The instability theory of drumlin formation applied to Newtonian viscous ice of finite depth. Proceedings of Royal Society, A, Mathematical, Physical and Engineering Sciences, 298 (2121), 2673-2694.

Greenwood, S.L. and Clark, C.D. (2010). The extent to which substrate lithology exerts a control on the distribution and size of subglacial bedforms. Sedimentary Geology, 232 (3-4), 130-144.

External Collaborators

  • Professor Chris Clark (University of Sheffield, UK)
  • Dr Paul Dunlop (University of Ulster, N. Ireland)
  • Professor Andrew Fowler (University of Limerick, Ireland)
  • Dr Richard Hindmarsh (British Antarctic Survey, UK)
  • Dr Heiki Gramberg (University of Oxford, UK)
  • Dr Felix Ng (University of Sheffield, UK)
  • Dr Matteo Spagnolo (University of Aberdeen, UK)

Project External Website

http://www.sheffield.ac.uk/drumlins/

Staff

From the Department of Geography