Subglacial bedforms

A generic term for the range of longitudinal and transverse landforms produced at the base of a glacier or ice sheet as a result of active ice flow across a sediment base.

Nigardsbreen glacier, Norway
Nigardsbreen glacier, Norway. Credit: Dr Darrel Swift.

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Whilst individual types of subglacial landforms have often been investigated in isolation, there has been an increasing realisation that they all belong to a single family of related landforms, best thought of as a continuum of subglacial bedforms (Rose, 1987).

This view uses the concept of a single set of processes that may lead to a wide range of landform shapes and characteristics, only some of which conform to our "classical text book" landform types such as the drumlin.

As with aeolian and fluvial bedforms one would expect a combination of distinctive landforms and a range of intermediate morphologies.


Specific landform types that are part of the subglacial bedform system are: flutes, drumlins and mega-scale glacial lineations, which are all longitudinally streamlined landforms at different scales from metres to tens of kilometres, and are commonly referred to as glacial lineations.

Rogen or ribbed moraine are also subglacial bedforms but are sculptured ridges formed transverse to the ice flow direction.

A strong characteristic of all subglacial bedforms are that that they occur in discrete and fairly well defined fields or swarms comprising hundreds to thousands of individuals, and that different types such as drumlins and Rogen moraine are often found in close association with each other.

An alternative school of thought considers that subglacial bedforms arise from large subglacial flood events, with water rather than ice being the shaping media. (See drumlin definition page for more information).


Reading

Benn, D.I., and Evans, D.J.A., 1998: Glaciers and Glaciation. London: Arnold.
Rose, J. 1987. Drumlins as part of a glacier bedform continuum. In Menzies, J. and Rose, J. (eds), Drumlin Symposium. Rotterdam, Balkema, 103-116.

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