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...

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Bibliographic Details
Published in:Earth Surface Processes and Landforms
Main Author: Robertson‐Rintoul, M. S. E.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1986
Subjects:
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