Stagnation or Activity in the Last Ice Remnants?
- 1 October 1981
- journal article
- Published by Taylor & Francis in Geografiska Annaler: Series A, Physical Geography
- Vol. 63 (3-4) , 139-147
- https://doi.org/10.1080/04353676.1981.11880027
Abstract
The age relationships between Rogen moraine ridges in the Central Swedish mountains and subglacially engorged valley side eskers on the mountain slopes are discussed. The movement rates of the downwasting ice remnants within the final ice-divide area must have decreased or partly ceased already when the eskers were formed on the hillsides. The drumlinization of the Rogen type ridges thus occurred at a stage prior to the disappearance of the ice bodies between the valley sides.Keywords
This publication has 3 references indexed in Scilit:
- Äke SundborgGeografiska Annaler: Series A, Physical Geography, 1987
- Studien zur Geomorphologie und zum letztglazialen Eisrückzug in den Gebirgen Süd-Lapplands, Schweden. Mit einer Geomorphologischen Übersichtskarte im Masstab 1:250 000Geografiska Annaler: Series A, Physical Geography, 1974
- Eskers near the Casement Glacier, AlaskaGeografiska Annaler: Series A, Physical Geography, 1966