Articles | Volume 67, issue 1
https://doi.org/10.5194/egqsj-67-25-2018
https://doi.org/10.5194/egqsj-67-25-2018
Express report
 | 
28 Aug 2018
Express report |  | 28 Aug 2018

Disestablishing “Glacial Lake Speight”, New Zealand? An example for the validity of detailed geomorphological assessment with the study of mountain glaciations

Stefan Winkler, David Bell, Maree Hemmingsen, Kate Pedley, and Anna Schoch

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Cited articles

Barrell, D. J. A., Andersen, B. G., and Denton, G. H.: Glacial geomorphology of the Central South Island, GNS Science Monographs, 27, Lower Hutt, New Zealand, 2011. 
Borsellino, R., Shulmeister, J., and Winkler, S.: Glacial geomorphology of the Brabazon and Butler Downs in the Rangitata Valley, New Zealand. J. Maps, 13, 502–510, https://doi.org/10.1080/17445647.2017.1336122, 2017. 
Brardinoni, F., Picotti, V., Maraio, S., Bruno P. P., Cucato, M., Morelli, C., and Mair, V.: Postglacial evolution of a formerly glaciated valley: Reconstructing sediment supply, fan building, and confluence effects at the millennial time scale, online first, Geol. Soc. Am. B., https://doi.org/10.1130/B31924.1, 2018. 
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Geomorphological mapping and analysis conducted as an initial step towards a future sediment budget study of the middle Waimakariri River (Southern Alps, New Zealand) reveals that the traditional concept of the temporary palaeolake glacial Lake Speight is conflicting with our conclusions of realistic chronosequences and timescales of para- and postglacial landform development. Especially the temporal and causal relation to the last deglaciation needs to be questioned and will be discussed.