The influence of rock mass strength on glacial valley cross‐profile morphometry: A case study from the Southern Alps, New Zealand
- 1 February 1992
- journal article
- Published by Wiley in Earth Surface Processes and Landforms
- Vol. 17 (1) , 39-51
- https://doi.org/10.1002/esp.3290170104
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- A discussion of hirano and Aniya's (1988, 1989) explanation of glacial‐valley cross profile developmentEarth Surface Processes and Landforms, 1990
- A reply to ‘a discussion of hirano and Aniya's (1988, 1989) explanation of glacial valley cross profile development’ by Jonathan M. HarborEarth Surface Processes and Landforms, 1990
- A rational explanation of cross‐profile morphology for glacial valleys and of glacial valley development: A further noteEarth Surface Processes and Landforms, 1989
- A rational explanation of cross‐profile morphology for glacial valleys and of glacial valley developmentEarth Surface Processes and Landforms, 1988
- A numerical model of landform development by glacial erosionNature, 1988
- Identification of strength equilibrium rock slopes: Further statistical considerationsEarth Surface Processes and Landforms, 1987
- Using parabolas to describe the cross‐sections of glaciated valleysEarth Surface Processes and Landforms, 1984
- Refinement of a technique for determining rock mass strength for geomorphological purposesEarth Surface Processes and Landforms, 1984
- The Role of the Ice Contributing Area in the Morphology of Transverse Fjords, British ColumbiaGeografiska Annaler: Series A, Physical Geography, 1984
- The Geomorphology of the Glacial Valley Cross SectionArctic and Alpine Research, 1970