Weichselian ice movement in South Norway and adjacent areas
Three main phases of ice‐movement pattern in South Norway during the Weichselian are reconstructed. During Phase II (possibly of Middle Weichselian age) the ice divide was located far to the west. Phase III (assumed Middle/Late Weichselian age) had an easterly situated ice divide. During Phase IV (P...
Published in: | Boreas |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1977
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Subjects: | |
Online Access: | http://dx.doi.org/10.1111/j.1502-3885.1977.tb00292.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1977.tb00292.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1977.tb00292.x |
Summary: | Three main phases of ice‐movement pattern in South Norway during the Weichselian are reconstructed. During Phase II (possibly of Middle Weichselian age) the ice divide was located far to the west. Phase III (assumed Middle/Late Weichselian age) had an easterly situated ice divide. During Phase IV (Preboreal age) the ice divide had moved back to the west and had partly fragmented into separate domes. The migration of the ice divide from west to east may be due to glacier surges, whilst the ice‐divide migration from Phase III to IV was probably a result of a general reduction in size of the ice sheet. |
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