Data relating to the collection of CRN samples from boulders on moraines on the lower flanks of the Butler and Brabizon Downs in the Rangitata Valley New Zealand. The study aimed to test whether the moraines related to one or many glacial advances and recessions. The study in QSR shows that the moraine sequence on the lower flank of the valley relates to a retreat of a single glacier at the end of the last ice age. It shows gradual ice evacuation from this area between c 21 and c 17 ka
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
The extent of Late Quaternary glaciation in the northwest Nelson region of New Zealand has tradition...
Data relating to the collection of CRN samples from boulders on moraines on the lower flanks of the ...
A suite of cosmogenic radionuclide ages taken from boulders on lateral and latero-terminal moraines ...
Four data sets. 1. A photographic archive of a selection of boulders used for CRN dating in the Rang...
New Zealand glaciers reached their last glacial maximum position at or before ~ 25 ka, and, as early...
This thesis presents stratigraphic, sedimentological and geochronological results from valley fill a...
We present Be-10 and Al-26 chronologies from the paleo-Rakaia glacier and the Clearwater lobe of the...
This thesis analyses the glacier fluctuations in New Zealand since late Pliocen until today (2017) a...
The inland valleys of New Zealand’s South Island were heavily glaciated during the last glacial cycl...
The extent of Late Quaternary glaciation in the northwest Nelson region of New Zealand has tradition...
Understanding natural climate variability is a fundamental goal of paleoclimate science. Temperate m...
A study of the glacial geology and present and past snowlines of tributaries to the Waimakariri Rive...
A 110 m thick succession of glacial valley fill is described from Poplars Gully, central South Islan...
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
The extent of Late Quaternary glaciation in the northwest Nelson region of New Zealand has tradition...
Data relating to the collection of CRN samples from boulders on moraines on the lower flanks of the ...
A suite of cosmogenic radionuclide ages taken from boulders on lateral and latero-terminal moraines ...
Four data sets. 1. A photographic archive of a selection of boulders used for CRN dating in the Rang...
New Zealand glaciers reached their last glacial maximum position at or before ~ 25 ka, and, as early...
This thesis presents stratigraphic, sedimentological and geochronological results from valley fill a...
We present Be-10 and Al-26 chronologies from the paleo-Rakaia glacier and the Clearwater lobe of the...
This thesis analyses the glacier fluctuations in New Zealand since late Pliocen until today (2017) a...
The inland valleys of New Zealand’s South Island were heavily glaciated during the last glacial cycl...
The extent of Late Quaternary glaciation in the northwest Nelson region of New Zealand has tradition...
Understanding natural climate variability is a fundamental goal of paleoclimate science. Temperate m...
A study of the glacial geology and present and past snowlines of tributaries to the Waimakariri Rive...
A 110 m thick succession of glacial valley fill is described from Poplars Gully, central South Islan...
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
Stratigraphic evidence and extensive optically stimulated luminescence (OSL) geochronology from an 1...
The extent of Late Quaternary glaciation in the northwest Nelson region of New Zealand has tradition...