A quantitative soil‐stratigraphic approach to the correlation and dating of post‐glacial river terraces in Glen Feshie, western Cairngorms
Abstract Little is known about Holocene river terrace development in upland Scottish valleys. Interpretation of many of the terrace sequences, previously suggested to have been formed by meltwaters either from the last Scottish ice sheet or the Loch Lomond Advance, has generally been based on morpho...
Published in: | Earth Surface Processes and Landforms |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1986
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Online Access: | http://dx.doi.org/10.1002/esp.3290110604 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290110604 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290110604 |