Mega‐scale glacial lineations and cross‐cutting ice‐flow landforms
Abstract Landsat images reveal a previously unsuspected large‐scale pattern of streamlining within drift that is assumed to reflect former phases of ice flow. Such a glacial grain can be regarded as a landform assemblage comprised of a number of components. Drumlins and megaflutes form part of the p...
| Published in: | Earth Surface Processes and Landforms |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Wiley
1993
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| Online Access: | http://dx.doi.org/10.1002/esp.3290180102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290180102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290180102 |
| Summary: | Abstract Landsat images reveal a previously unsuspected large‐scale pattern of streamlining within drift that is assumed to reflect former phases of ice flow. Such a glacial grain can be regarded as a landform assemblage comprised of a number of components. Drumlins and megaflutes form part of the pattern, but in addition there are two previously undocumented ice‐moulded landform elements: streamlined lineations of much greater proportions, referred to as mega‐scale glacial lineations, and a distinctive cross‐cutting topology within the grain. The ice‐moulded landform assemblage is described and illustrated with reference to examples from Canada. Possible modes of genesis of such landforms are discussed and their glaciological implications outlined. The discovery of this pattern indicates the pervasive nature of subglacial deformation of sediment, and demands a radical re‐interpretation of ice sheet dynamics. |
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