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...

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Bibliographic Details
Published in:Boreas
Main Author: VORREN, TORE O.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1977
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
Description
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.