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DOI | 10.1016/j.quascirev.2019.03.035 |
Ice-contact proglacial lakes associated with the Last Glacial Maximum across the Southern Alps; New Zealand | |
Sutherland J.L.; Carrivick J.L.; Shulmeister J.; Quincey D.J.; James W.H.M. | |
发表日期 | 2019 |
ISSN | 0277-3791 |
起始页码 | 67 |
结束页码 | 92 |
卷号 | 213 |
英文摘要 | Proglacial lakes can affect the stability of mountain glaciers and can partly disengage glacier behaviour from climatic perturbations. However, their role in controlling the onset and progression of deglaciation from the Last Glacial Maximum (LGM) remains poorly understood. This lack of understanding is partly because the evidence required to consistently and robustly identify the location and evolution of ice-contact lakes is not standardised. In this paper we therefore firstly present a new set of criteria for identifying the landform and sedimentary evidence that defines and characterises ice-marginal lakes. Secondly, we then apply these key criteria with the aid of high-resolution topographic mapping to produce the first holistic definition and assessment of major proglacial lake landforms and sediments pertaining to the end of the LGM across South Island, New Zealand. The major findings of this assessment can be grouped to include that: (i) The localised constraints to proglacial lake extent were topography, glacier size and meltwater/sediment fluxes, (ii) Lake damming was initiated by outwash fan-heads that interrupted water and sediment flows down-valley, and (iii) New Zealand LGM lakes were unequivocally in contact with a calving ice margin. These findings will be useful for reconstructing ice dynamics and landscape evolution in this region. © 2019 |
英文关键词 | Airborne LiDAR; DEM; Glacial geomorphology; Glaciation; Glaciolacustrine; Last Glacial Maximum; LGM; New Zealand; Proglacial lake; Quaternary; Southern pacific |
语种 | 英语 |
scopus关键词 | Geomorphology; Glacial geology; Lakes; Landforms; Sediments; Topography; Airborne LiDAR; Glacial geomorphology; Glaciation; Glaciolacustrine; Last Glacial Maximum; New zealand; Proglacial lakes; Quaternary; Southern pacific; Ice; airborne survey; climate change; deglaciation; digital elevation model; fluvial geomorphology; glacial lake; glaciation; glacier; glaciolacustrine deposit; ice; landscape evolution; Last Glacial Maximum; lidar; mountain environment; periglacial landform; Quaternary; reconstruction; sediment-water interface; topographic mapping; New Zealand; Pacific Ocean; Pacific Ocean (South); South Island; Southern Alps |
来源期刊 | Quaternary Science Reviews |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151933 |
作者单位 | School of Geography and Water@leeds, University of Leeds, Woodhouse Lane, Leeds, West Yorkshire LS2 9JT, United Kingdom; School of Earth and Environmental Sciences, University of Queensland, St Lucia, Queensland 4072, Australia |
推荐引用方式 GB/T 7714 | Sutherland J.L.,Carrivick J.L.,Shulmeister J.,et al. Ice-contact proglacial lakes associated with the Last Glacial Maximum across the Southern Alps; New Zealand[J],2019,213. |
APA | Sutherland J.L.,Carrivick J.L.,Shulmeister J.,Quincey D.J.,&James W.H.M..(2019).Ice-contact proglacial lakes associated with the Last Glacial Maximum across the Southern Alps; New Zealand.Quaternary Science Reviews,213. |
MLA | Sutherland J.L.,et al."Ice-contact proglacial lakes associated with the Last Glacial Maximum across the Southern Alps; New Zealand".Quaternary Science Reviews 213(2019). |
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