Regional variation in the composition of Neoglacial end moraines, Jotunheimen, Norway: an altitudinal gradient in clast roundness and its possible palaeoclimatic significance
- 1 June 1987
- Vol. 16 (2) , 173-188
- https://doi.org/10.1111/j.1502-3885.1987.tb00769.x
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- The Detection of High Altitude Permafrost in Jotunheimen, Norway Using Seismic Refraction Techniques: An AssessmentArctic and Alpine Research, 1986
- Glacial geomorphologyProgress in Physical Geography: Earth and Environment, 1984
- A method for determining total clast roundness in sedimentsBoreas, 1983
- Genesis of marginal moraines in the CaucasusBoreas, 1982
- Within‐valley asymmetry and related problems of Neoglacial lateral moraine development at certain Jotunheimen glaciers, southern NorwayBoreas, 1982
- Depositional processes of Pleistocene lowland end Moraines, and their possible relation to climatic conditionsBoreas, 1982
- Glacier and climatic fluctuations inferred from tree‐growth variations over the last 250 years, central southern NorwayBoreas, 1977
- ‘Little Ice Age’ palaeotemperatures from high altitude tree growth in S. NorwayNature, 1976
- Hydrologie et érosion sous-glaciairesJournal of Alpine Research | Revue de géographie alpine, 1970
- A New Roundness Scale for Sedimentary ParticlesJournal of Sedimentary Research, 1953