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1. Assessment of the rate of contaminant movement through Antarctic soils using a lithium chloride experiment at Lake Vanda [K150_1993_1994_NZ_4]
A leaching trial was set up at Lake Vanda to determine how rapidly and how far water-soluble materials spilt on the soil surface will move. A series of 1 x 1 m plots and control sites on the north ...


2. Baseline information on both the modern processes operating on Antarctic beaches and the development of beach ridges in relation to the last glaciation ice retreat and isostatic rebound [K043_1996_1998_NZ_1]
Beaches in McMurdo Sound have developed since the last glaciation when ice sheets were at their maximum. The weight of the overlying ice, depressed the land, which has slowly rebounded forming a series ...


3. Biochemical and biological activity of soils from a penguin colony at Cape Bird and soil description, classification and measurements of water content, soil temperature and depth to frozen ground [K024_1981_1984_NZ_1]
The biochemical and biological activity of the soils of the Adelie penguin colonies at Cape Bird was studied over two seasons. Biochemical markers of decomposition of penguin guano were studied by ...


4. Biological soil samples from a range of salty hollows to determine if some life forms had adapted to this environment [K150_1987_1988_NZ_1]
Soil biological samples were collected from a range of salty hollows to determine if some life forms had adapted to this environment because biological adaptation in Antarctica is such that virtually ...


5. Biostratigraphic collections of Devonian fish fossils from Middle Devonian Aztec Siltstone at the top of the Taylor Group (Beacon Supergroup) and sediment studies for a basin analysis [K026_1991_1992_NZ_1]
Using toboggans and sledges, the party travelled 700 kilometres from the Darwin Glacier northwards to the Lashly Mountains to study Taylor Group sedimentary rocks (Beacon Supergroup). The principle ...


6. Monitoring of permafrost temperatures at Marble Point and Bull Pass, Wright Valley [K123_2005_2007_NZ_1]
Bore holes were drilled in bedrock near existing climate monitoring stations at Marble Point and Bull Pass, Wright Valley to monitor permafrost temperatures at depths of up to 30m and to drill till ...


7. Profile descriptions, mapping and analysis of soils in the Wright Valley, Antarctica and assessment of soil disturbance by foot traffic [K123_2004_2005_NZ_1]
Soil profile descriptions from the Lower Wright Valley, West Wright Valley (including north and south forks), Labyrinth and Dais was carried out over three field seasons (2004-05, 2005-06 and 2006-07) ...


8. Provenance analysis of Cambrian conglomerates, Northern Victoria Land [K051_2000_2003_NZ_1]
The Cambrian volcanic arc of North Victoria Land and the Cambrian arc of NW Nelson (NZ) are strikingly similar. They are of island arc character but both now lie within continental crust. In NVL ...


9. Petrology and geochemistry of alkaline and granitoid intrusions, Pipecleaner Glacier region, southern Victoria Land, Antarctica [K061_1989_1990_NZ_2]
The primary aim was to extend the field mapping, undertaken by previous MSc students from Otage University in Southern Victoria Land. The area mapped included the Miers Valley and around the Pipecleaner ...


10. Oceanography and sedimentation beneath the McMurdo/Ross Ice Shelf in Windless Bight [K042_2002_2003_NZ_1]
Water flow and sedimentation beneath the McMurdo Ice Shelf south of Ross Island was investigated by using a hot water drilling system to melt access holes through the ice shelf allowing measurements ...


11. Oceanography, sea seismic surveys and benthic surveys of the New Zealand sub-Antarctic Islands areas (Auckland and Campbell Islands), the Macquarie Ridge area and the ocean between New Zealand and the Ross Sea [K002_1959_1963_NZ_1]
Oceanographic, sea seismic surveys and benthic surveys were conducted aboard research vessels (HMNZS Endeavour, Wilhoite, Rotoiti, USS Burton Island) between 1959 and 1963. The principal aim of the ...


12. Palaeomagnetic measurements of red bed Beacon Supergroup rocks (Terra Cotta Siltstone and Aztec siltstone) samples from South Victoria Land [K042_1980_1981_NZ_3]
It had been previously found that sampled rocks from Beacon sandstones at Mt Bastion, Beacon Heights and Table Mountain were very weakly magnetised and their magnetic direction had been reset at the ...


13. Palaeomagnetic measurements on rocks from Mt Crean to determine the continental drift of gondwanaland [K045_1994_1995_NZ_1]
The Beacon sediments of East Antarctica were deposited over the Devonian to Triassic geological periods, from 400 to 200 million years ago. Palaeomagnetic measurements on these rocks provide information ...


14. Palaeozoic Terrane Correlation: New Zealand and Antarctica [K051_2003_2004_NZ_2]
In St Johns Range and eastern Olympus Range, unusually coarse lithologies at the base of the Beacon Supergroup have the potential to provide significant information on the provenance of the earliest ...


15. Paleomagnetic samples and geological mapping of the basement geology of the Daniels Range and the Rennick Glacier area in North Victoria Land [K017_1981_1982_NZ_1]
A collection of paleomagnetic rock samples including Jurassic volcanics and dolerites, Beacon Supergroup, Devonian-Carboniferous volcanics, Paleozoic Granitoids and Cambrian Volcanics and sediments ...


16. Paleozoic tectonics of the Gondwana margin: Provenance of the Sperm Bluff Conglomerate. Implications for Cambrian tectonics and Devonian and younger paleotectonics and paleogeography [K051_2003_2004_NZ_1]
The basement rocks of eastern Northern Victoria Land (NVL) consist of a series of exotic terrances that were accreted to the Gondwanan margin while Andean style convergence was occurring. Conversely, ...


17. Petrological evolution of basement granitoids Southern Victoria Land, Antarctica [K061_1986_1987_NZ_1]
Several workers have studied the basement and other granitoids in the Dry Valleys, without a detailed petrographical and chemical study of these rocks. This study was aimed at elucidating the evolution ...


18. Petrology of Koettlitz Group meto-sediments and gneisses from the mid Taylor Valley and mid Ferrar Glacier areas [K061_1986_1987_NZ_3]
Highly deformed Koettlitz Group rocks from the mid Taylor Valley, Dun Glacier and Catherdral Rocks areas contain migmatitic and non-migmatitic gneisses of unknown parentage. Detailed mapping and examination ...


19. Rb-Sr dating of Asgard Formation rocks from the Lower Wright Valley and Victoria Valley to determine the age of the oldest basement rocks in the Ross Dependency [K231_1985_1986_NZ_1]
A programme was conducted to determine the age of the oldest basement rocks in the Ross Dependency. The Asgard Formation in the Dry Valleys is a series of metamorphosed sedimentary rocks that form ...


20. Reconnaissance of the Balleny Islands [K017_1963_1964_NZ_1]
A reconnaissance expedition took place around the Balleny Islands in the 1963-1964 field season with the objective to examine the four beaches where landings had previously been made and to search ...


21. Regional stratigraphy, sedimentology structure, metamorphic and tectonic history of the lower grade Skelton Group meta-sediments between the Skelton and Koettlitz Glaciers [K002_1975_1976_NZ_1]
A study of the low grade meta-sedimentary rocks of the Skelton and Koettlitz Glacier areas including the unmapped Mt Cocks Range at the head of the Koettlitz Glacier was investigated to add to the ...


22. Rock Samples for Cosmogenic Dating from the Darwin Glacier area [K056_2006_2007_NZ]   PARENT DIF
Rocks were Collection of rock samples from the Darwin glacier area for cosmogenic dating and the data tables contain technical data required for cosmogenic dating analysis.


23. Rock samples for fission track dating from several locations along the Victoria Land coast, used to obtain rates of uplift and vertical movement of the Transantarctic Mountains [K043_1983_1986_NZ_1]
The study of mountain uplift using fission-track dating techniques requires sampling at regular intervals over significant elevation ranges in order to gain information representing the greatest possible ...


24. Salt, nutrient and other contaminant analysis of soil samples taken near the old Vanda Station [K105_1993_1994_NZ_2]
Water and soil samples from Vanda Station were found to have contamination by apparently anthropogenically derived components (such as heavy metals) and these contaminants are moving in the soils ...


25. Sampling petroleum contaminated soils for microbes at the historic huts [K021_1998_2008_NZ_8]
Soil samples were taken at Cape Evans where the remains of 2 petroleum depots are located near the hut (1999-2000 season) to ascertain if hydrocarbons were present. Additional sampling was carried ...


26. Sea ice cracks, sea ice movement and tide movements of Granite Harbour [K042_1982_1983_NZ_4]
Active spreading sea ice cracks were found in the sea ice of Granite Harbour over several seasons. The cracks would prove difficult for heavy surface transport required for a drill rig site establishment. ...


27. Seasonal soil temperature and moisture data from a site in Marble Point [K150_1991_1992_NZ_3]
Seasonal behaviour of soil water content cannot be determined from short term periodic site observations but instead by continuous monitoring. In order to attempt to look at this question, a datalogger ...


28. Sediment cores from Lakes Fryxell, Lake Bonney and Lake Joyce, in the McMurdo Dry Valleys, Antarctica [K022_2002_2003_NZ_1]   PARENT DIF
Cores were taken from lakes in the McMurdo Oasis to identify and date periods of low lake level to add to the existing record of periods of high lake level, with the intention of comparing the isotopic ...


29. Sediment transport load in the Onyx River, Wright Valley [K164_1984_1985_NZ_1]
The sediment transport load in the Onyx River was investigated. The bedload transport rates were used in association with the 15 year flow record, to estimate sandur sedimentation rates. 38 cross ...


30. Sedimentological and palaentological examination of the Devonian Horlick formation in the Ohio Range of the Horlick Mountains [K026_1979_1980_NZ_1]
15 sections of the Horlick formation were measured in detail along the Ohio escarpment from Discovery Ridge to Lackey Ridge. The Ohio Range contains the only well exposed record of unequivocally marine ...


31. Sedimentological and structural measurements and rock samples for radiometric dating of the Swanson Group and Ford Granodiorite of the Ford Ranges, Marie Byrd Land, West Antarctica [K051_1978_1979_NZ_1]
The purpose of the expedition was to examine in detail the pre-Cenozoic geology of the Ford Ranges which comprise the main area of exposed rock in western Marie Byrd Land and the type area of two ...


32. Seismic and sedimentological studies of the seafloor in the Cape Hallett region [K041_1986_1987_NZ_2]
Sediment transport in several large submarine channels, that cross the Cape Hallett region, with subsequent deposition in the basins to the north was investigated. Two parallel single channel seismic ...


33. Seismic profile survey of McMurdo Sound and Terra Nova Bay [K042_1974_1975_NZ_2]
As part of the Dry Valleys Drilling Project, the area of the McMurdo Sound drill hole was surveyed with a seismic survey profile and extended to cover the whole of the McMurdo Sound region to determine ...


34. Seismic reflection data from a 50km line southeast of the summit of Mt Erebus to assess the amplitude and wavelength of crustal flexure associated with the load of the Ross Archipelago [K101_1988_1989_NZ_1]
A joint project between the New Zealand Geophysic Division (now IGNS), Stanford University and the University of Nebraska was conducted to carry out a seismic reflection line of approximate 50 km ...


35. Seismic reflection survey across Hut Point Peninsula to determine the sedimentary sequence under the peninsula to define Cenozoic glacial and volcanic history of the region [K101_1992_1993_NZ_1]
A seismic reflection survey and wide angle reflection experiment was carried out along an 11km profile, starting approximately 8 km east of Hut Point Peninsula and heading west to delineate the sedimentary ...


36. Seismic refraction and reflection measurements of the east-west Antarctic plate boundary near the Lowery Glacier and onto the Ross Ice Shelf, south Victoria Land [K101_1990_1991_NZ_1]
In the 1990-1991 season, a seismic refraction and reflection experiment was completed along a 142 km long line across the transition zone between Ross Embayment and the Transantarctic Mountains, just ...


37. Seismic refraction surveys in the McMurdo Sound region [K042_1964_1965_NZ_5]
The suitability of first arrival seismic refraction apparatus for surface structure studies was investigated at sites in the Wright, Taylor and Miers Vallyes and on Brown Peninsula. Results show that ...


38. Seismic, bathymetry and piston coring transects to determine sediment movement in the Cape Royds area [K041_1986_1987_NZ_3]
Seismic, bathymetry and piston coring transects were undertaken in the Cape Royds area to determine how sediment was moving over the sea floor of this area to the 900m deep Erebus basin offshore. ...


39. Seismic, gravity, radar and magnetic measurements across the East Antarctic ice sheet from the Transantarctic Mountains to the Wilkes sub-glacial basin [K101_1993_1994_NZ_1]
A geophysical traverse, designed to image the sedimentary layer under the 3 km thick East Antarctic ice sheet, was completed across part of East Antarctic ice cap west of McMurdo Sound. The programme ...


40. Seismic, infrasonic and magnetic induction data from Mt Erebus: 1980-1986, The International Mt Erebus Seismci Survey (IMESS) [K044_1980_1986_NZ_1]
The International Mt Erebus Seismic Survey (IMESS) was conducted on Mt Erebus to monitor and assess the seismic activity of the volcano year round. Seismic, infrasonic and magnetic induction data ...


41. Seismograph data from the David Glacier region near Terra Nova Bay to determine the origins of low magnitude seismicity in the area: brittle ice failure, basal shearing beneath the glacier, or tectonic events? [K101_2003_2004_NZ_1]
Temporary seismograph stations placed in the Transantarctic Mountains have recorded regular, low magnitude seismicity. The origin of the quakes could not be uniquely discriminated among brittle ice ...


42. Short term climate measurements and permafrost and soil moisture content of coastal mountain zones: Coombs Hills, Convoy Range and Asgard Range [K150_1994_1995_NZ_1]
Permafrost and soil moisture properties were measured at 15 sites in the Coombs Hills and Northwind Glacier and from 2 additional sites in the Asgard Range and the lower Barwick Valley to determine ...


43. Snow pit sampling and ice cores (from Dome C) used to measured the cosmogenic radionucleide 32Si for depositional variation and determination of half life for radiometric dating methods [K110_2003_2004_NZ_1]
Ice core records are very useful for determining past climate because they store a wide variety of proxies for climate forcing and climate response. Accurate dating of ice cores is crucial to making ...


44. Soil albedo measurements of oil-contaminated and control sites at Scott Base and Marble Point [K123_2000_2001_NZ_1]
Soil albedo measurements were made on oil contaminated and pristine soil surfaces at Scott Base and Marble Point using a single LI200X Pyranometer facing upward and downward to detect incoming and ...


45. Soil and groundwater description, characterisation and sampling at various sites at Cape Hallett [K123_2003_2005_NZ_1]
The soil and groundwater at Seabee Hook, Cape Hallet was described and characterised. Soil Investigation: Soil pits were dug east of Willett Cove on low mounds on disturbed and undisturbed sites, ...


46. Soil and salt samples and geological observations from high altitude sites in the Upper Taylor Valley to determine the history of the Antarctic environment through the composition of salts in soils [K105_1997_1998_NZ_1]
To understand the processes of Antarctic soils as they affect the composition and distributions of salts and ice in and below the soils, the salts in very old soils and paleosols were investigated. ...


47. Soil chemistry and soil CO2 concentration and isotopic composition from sites in Taylor Valley and the Lake Wellman area [K072_2008_2010_NZ_1]
This study aimed to understand the origin and dynamics of pedogenic carbonate in Antarctic soils, with a long-term view to understanding the formation of carbonate and the storage and turnover of ...


48. Soil climate and atmospheric data for Scott Base, Marble Point, Mount Fleming, Bull Pass, Granite Harbour, Minna Bluff and the Victoria Valley, Antarctica [K123_1999_2008_NZ_1]
In collaboration with the United States Department of Agriculture (USDA) climate stations were installed at six locations in the Ross Sea Region including Scott Base, Marble Point and Bull Pass all ...


49. Soil climate and atmospheric data for Scott Base, Marble Point, Mount Fleming, Bull Pass, Granite Harbour, Minna Bluff, Victoria Valley, Don Juan Pond and Bull Pass, Antarctica [K123_1999_2012_NZ_1]
In collaboration with the United States Department of Agriculture (USDA) climate stations were installed at six locations in the Ross Sea Region including Scott Base, Marble Point and Bull Pass all ...


50. Soil pit description and analysis (thin sections, cation and anion chemistry of soluble salts) from Beacon, Arena and Pearce Valley to determine the origin of ground ice at high elevations in the Dry Valleys [K047_2001_2002_NZ_1]
The origin of ground ice at high elevations (>1000m) throughout the Dry Valleys of Antarctica was investigated as the origin is unclear because there is no obvious comtemporary source of water. A ...


Showing 1 through 50 of 331 Next

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