Geomorphological contrast between advance and retreat phases at the terminus of a dynamic maritime glacier: Fox Glacier/Te Moeka o Tūwae, New Zealand (2020)

Type of Content
Conference Contributions - OtherCollections
Citation
Purdie H, Bealing P, Gomez C, Anderson B, Marsh O (2020). Geomorphological contrast between advance and retreat phases at the terminus of a dynamic maritime glacier: Fox Glacier/Te Moeka o Tūwae, New Zealand. Matiu/Somes Island, Wellington: Snow and Ice Research Group (SIRG) workshop. 03/02/2020-05/02/2020.This citation is automatically generated and may be unreliable. Use as a guide only.
ANZSRC Fields of Research
37 - Earth sciences::3709 - Physical geography and environmental geoscience::370902 - Glaciology37 - Earth sciences::3709 - Physical geography and environmental geoscience::370901 - Geomorphology and earth surface processes
Rights
All rights reserved unless otherwise statedRelated items
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Bathymetric and terminus evolution as determined by remote-sensing techniques: Tasman Glacier, New Zealand
Purdie, H.; Bealing, P.; Tidey, E.; Gomez, C. (University of Canterbury. Geography, 2015)Global glacier recession is increasing the number of glaciers that terminate in proglacial lakes, yet knowledge about the processes that drive ice-berg calving are still poorly understood. This knowledge-gap is in part due ... -
Rockfall at Fox Glacier, New Zealand: a Hazard Analysis using Structure from Motion and Spatial Modelling
Roy, E.S.; Purdie, H.; Gomez, C.; Wassmer, P.; Schuster, M. (University of Canterbury. Geography, 2015)As glaciers retreat, downwasting of the ice increases the instability of surrounding rock slopes. In addition, ice thinning can lead to surface morphology changes that can result in a progressively concave transverse ...