Glacial geology
; Landforms
; Cosmogenic radionuclides
; Data support
; Deglaciations
; Glacial ice
; Proglacial lakes
; South Island
; South Island , New Zealand
; Terminal moraines
; Ice
; boulder
; cosmogenic radionuclide
; deglaciation
; glacier dynamics
; ice retreat
; late glacial
; moraine
; proglacial environment
; valley
; volume change
; warming
; Canterbury [South Island]
; New Zealand
; Rakaia Valley
; Rangitata River
; South Island
; South Island
School of Earth and Environmental Sciences, University of Queensland, St Lucia, QLD 4072, Australia; Australian Nuclear Science and Technology Organisation, Lucas Heights, Australia; Institut für Geographie und Geologie, Universität Würzburg, Am Hubland, Würzburg, D-97074, Germany; Department of Geosciences, Idaho State University, Pocatello, ID, United States; Primary Science Solutions LTD., Christchurch, New Zealand; Department of Geology, Utah State University, Logan, UT 84322-4505, United States
Recommended Citation:
Shulmeister J.,Fink D.,Winkler S.,et al. Evidence for slow late-glacial ice retreat in the upper Rangitata Valley, South Island, New Zealand[J]. Quaternary Science Reviews,2018-01-01,185