Genesis of late pleistocene cross‐valley moraine ridges, South—Central Ulster, Northern Ireland
Abstract Four genetic varieties of ice‐marginal cross‐valley moraine ridge have been identified in south‐central Ulster, Northern Ireland. Type I ridges are flat topped, composed of stratified, water‐lain sediments and formed by coalescence of a series of supraaquatic deltas. Type II ridges are shar...
Published in: | Earth Surface Processes and Landforms |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1985
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Online Access: | http://dx.doi.org/10.1002/esp.3290100507 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290100507 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290100507 |