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8 Titles Match Your Query
Showing 1 through 8 of 8
1. Comparative studies of pebble and sediments from known sedimentary environments (Taylor Glacier, Table Mountain and Crary Ice Rise) with those found in a DVDP core [K042_1974_1975_NZ_1]
Examination of the cores from the Dry Valley Drilling Project consisted of, among other studies, grain size, pebble and magnetic investigations. Pebble and sediment sampling from known sedimentary ...


2. 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 ...


3. Geological mapping and investigations of the Permian Maya Erosion Surface, Metschel Tillite, Pre-Pleistocene tills and Wellar Coal Measures in the Upper Taylor Glacier area and Coombs Hills [K042_1977_1978_NZ_2]
Geological investigation in the upper Taylor Glacier was conducted and had three objectives; 1) To locate and examine at Kennar Valley, Finger Mountain and Mount Feather, within the Quartermain Mountains ...


4. 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 ...


5. Investigations of the accretion of ice at the base of dry based glaciers in the McMurdo Dry Valleys (Suess, Canada, LaCroix, Taylor, Lower Wright, Clark and Upper Victoria glaciers) [K064_1995_1996_NZ_1]
The process of ice accretion at the base of dry polar glaciers in the Dry Valleys of southern Victoria Land was examined. The Suess, Canada, LaCroix and Taylor glacier in the Taylor Valley, the Lower ...


6. The behaviour of dry based glaciers and the interpretation of Pleistocene glacial deposits from glaciers in the Dry Valleys, Antarctica [K064_1994_2005_NZ]   CHILD DIFs
The formation of deposits and landforms at the margin of alpine glaciers in the Dry Valleys (The Suess Glacier, Taylor Glacier and Rhone Glacier in the Taylor Valley, the Wright Lower Glacier in the ...


7. The structural glaciology and movement of the Taylor Glacier, Taylor Valley, Antarctica [K064_1994_2005_NZ_3]   PARENT DIF
The structural glaciology and movement of the Taylor Glacier, was investigated over several seasons (98-01) by excavating a tunnel in the right side of the Taylor Glacier, 1.5km upstream of the terminus, ...


8. Measurements of the effects of debris on the mechanical behaviour (deformation and motion) of ice of the Taylor Glacier, Taylor Valley, Antarctica [K053_1992_2000_NZ_1]
Debris-rich ice is a commonly observed basal ice facies found at the base of many temperate and polar glaciers and at the base of cores through major ice sheets. The effects of the presence of debris ...


Showing 1 through 8 of 8

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