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20 Titles Match Your Query
Showing 1 through 20 of 20
1. GIS analysis, biological samples (soil microorganism, invertebrate and plant), automatic weather station data and vegetation and invertebrate surveys to determine the terrestrial biocomplexity of the McMurdo Dry Valleys [K020_2008_2012_NZ_1]
The McMurdo Dry Valleys are the largest area of snow-free land in Antarctica. Managers ability to promote and protect these areas would benefit if we knew the biodiversity present and what controls ...


2. Dynamics and change of the Darwin Hatherton Glacial System [K056_2006_2010_NZ_1]   CHILD DIFs
The Darwin-Hatherton glacial system offers a unique opportunity to investigate the response of the Antarctic Ice Sheet to future climate change. As well as draining the East Antarctic Ice Sheet into ...


3. Geomorphological information from the Darwin-Hatherton area, Antarctica [K056_2006_2007_NZ_2]   PARENT DIF
Rock samples were collected from the Darwin Glacier region (6 samples) during the 06-07 season. Over 100 samples were collected from the Lake Wellman, Hatherton Glacier area during the 07-08 season. ...


4. Ground penetrating radar survey of the Darwin and Hatherton glacial systems [K056_2006_2007_NZ_3]
More than 300 km of ground penetrating radar (GPR) data were collected on the glaciers around Roadend Nunatak, Lake Wellman and Lake Wilson. Reflections from the bedrock were observed on most profiles, ...


5. Southern Victoria Land Geological Map, 1:250 000, GNS Science [K105_2008_2009_NZ_2]
Geological field observations collected from New Harbour, Kukri Hills, Ferrar Glacier, Bettle Peak, Blue Glacier, Mt Lister, Salmon Valley, Cape Chocolate and Walcott Bay; of basement rock, Beacon ...


6. GIS analysis, biological samples (soil microorganism, invertebrate and plant), automatic weather station data and vegetation and invertebrate surveys to determine the terrestrial biocomplexity of the McMurdo Dry Valleys [K020_2008_2009_NZ_1]
The McMurdo Dry Valleys are the largest area of snow-free land in Antarctica. Managers ability to promote and protect these areas would benefit if we knew the biodiversity present and what controls ...


7. The hydrology, glaciology and sediment transport monitoring of the glacial-river-lake system in the Miers Valley, Antarctica [K046_1988_1991_NZ_1]   PARENT DIF
A three year hydrological, glaciological and sediment transport monitoring programme was conducted in the Miers Valley. The energy and mass balances of the glacier-river-lake system was investigated ...


8. Using diamict and glacio-tectonised samples to determine previous glacial overriding in the Allan Hills nunatak [K042_1999_2000_NZ_1]
The character and form of previous glacial overriding in the Allan Hills nunatak was determined by describing and quantifying the glacio-tectonised bedrock from Sirius related glaciations. The Sirius ...


9. Detailed description, mapping and sampling (for sedimentology, paleontology and chronology studies) of Cenozoic bedded polymicton-type sediments within the Taylor Valley [K042_1974_1975_NZ_3]
Cenozoic bedded polymicton-type sediments within the Taylor Valley were mapped. These polymicton-type sediments are of glacial origin deposited into a body of water and therefore exhibit sorting and ...


10. Determination of deposition, sediment transport direction and age of New Mountain Sandstone (Beacon Supergroup) at various localities in the Royal Society Range and Dry Valleys region [K042_1974_1975_NZ_4]
The New Mountain Sandstone, the lowest formation of the Beacon Supergroup was studied in detail at various localities in the Royal Society Range and Dry Valley's region to determine its environment ...


11. Examination of the Cenozoic glaciomarine deposits, moraines and benches of Black Island and Brown Peninsula [K042_1975_1976_NZ_1]
Correlation of Cenozoic glaciomarine deposits, moraines and benches of Black Island and Brown Peninsula was conducted. Flat coastal areas at the north-western end of Black Island were found to consist ...


12. Geological investigation into the mode of origin of the Wright and Taylor Valleys [K042_1969_1970_NZ_2]
The Labyrinth area in the Wright Valley is an unusual area of very steep gullies with flat treads between, which form a box canyon type topography. The mode of origin of the area is a controversial ...


13. Investigation of the process of debris entrainment and till deposition of the Taylor Glacier [K042_1976_1977_NZ_1]
Investigations into the processes of debris entrainment and the formation of a debris layer within glacial ice was conducted. The glacial ice velocity at various points on the Taylor Glacier was conducted ...


14. Investigations of the glaciology and hydrology in the Terra Nova Bay regions [K162_1984_1985_NZ_1]
The occurrence or non-occurrence of both glacial moraines and past sea levels in the Terra Nova Bay area was investigated with a view to establishing a glacial chronology to supplement the Dry Valleys ...


15. Determination of the Sirius Group (Neogene deposits) mode of deposition at Allan Hills, Mt Feather and Table Mountain [K042_1997_2001_NZ_1]
An ancient glacial deposit termed the Sirius Group is a collection of Neogene deposits that crop out at high elevations throughout the Transantarctic Mountains (TAM). The paleoflow direction and how ...


16. The geology of the Northern Britannia Range between the Hatherton and Byrd Glaciers [K009_1978_1979_NZ_1]   PARENT DIF
The geology of the Northern Britannia Range between the Hatherton and Byrd Glaciers was mapped and the landforms, soils and glacial history of the range was investigated. A four man team man-hauled ...


17. The geomorphology of the Victoria Valley, the Wright Valley, the Koettlitz Valley and its tributaries and the Olympus Range [K009_1971_1972_NZ_1]   PARENT DIF
The research was concerned with several aspects of the geomorphology of the Victoria Valley, the Wright Valley, the Koettlitz Valley and its tributaries and the Olympus Range areas. Particular studies ...


18. Geochemistry investigations of landforms in the Ross Sea Region to determine past glacial history and landform processes [K009_1969_1970_NZ_1]   PARENT DIF
The geochemistry of Ross Island (Cape Barne and Cape Crozier), the Taylor and Wright Valleys, Lake Vida in Victoria Valley and Marble Point was studied (weathering and land formation) to determine ...


19. Analysis of shallow cores (stratigraphy, thickness and facies analysis, ageing) from Allan Hills and Table Mountain and assessment of contamination of diesel drilling fluid from DVDP-6 core, Lake Vida, 1972 [K047_2000_2001_NZ_1]
Shallow coring of permafrost glacial sediments was completed of the Sirius Group at Allan Hills to provide stratigraphic cores for thickness and facies analysis and at Table Mountain for comparative ...


20. Geological and geomorphic data and Sirius Group core analysis (stratigraphy, petrographical analysis, ground temperature and isotope analysis) from Table Mountain to determine the depositional history [K047_1996_1997_NZ_1]
The depositional and post depositional history of the Sirius Group tillite in the Dry Valleys area was investigated to resolve the ongoing debate as to whether the East Antarctic ice sheet formed ...


Showing 1 through 20 of 20

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