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Welcome to Glaciers @ Otago, Glaciers | glaciers.otago.ac.nz Reviews

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1

Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica, Glaciers

http://glaciers.otago.ac.nz/publications/form,_structure_and_stability_of_the_margin_of_the_antarctic_ice_sheet,_vestfold_hills_and_bunger_hills,_east_antarctica

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

2

Ice formation in an Antarctic glacier-dammed lake and implications for glacier-lake interactions, Glaciers

http://glaciers.otago.ac.nz/publications/ice_formation_in_an_antarctic_glacier-dammed_lake_and_implications_for_glacier-lake_interactions

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

3

Ice composition evidence for the formation of basal ice from later water beneath a cold-based Antarctic glacier, Glaciers

http://glaciers.otago.ac.nz/publications/ice_composition_evidence_for_the_formation_of_basal_ice_from_later_water_beneath_a_cold-based_antarctic_glacier

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

4

Supraglacial eskers in Antarctica, Glaciers

http://glaciers.otago.ac.nz/publications/supraglacial_eskers_in_antarctica

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

5

Direct shear tests of materials from a cold glacier: implications for landform development, Glaciers

http://glaciers.otago.ac.nz/publications/direct_shear_tests_of_materials_from_a_cold_glacier_implications_for_landform_development

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

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Welcome to Glaciers @ Otago, Glaciers

Thermal and mechanical processes at the beds of cold glaciers. Quaternary Geomorphology of the Southern Alps. Mass Balance of Glaciers. Mechanical behaviour and structure of the debris-rich basal ice layer. Ice-marginal terrestrial landsystems: polar continental glacier margins. Equifinality of basal ice facies from an Antarctic cold-based glacier. Form, structure and stability of the margin of the Antarctic ice sheet, Vestfold Hills and Bunger Hills, East Antarctica. Supraglacial eskers in Antarctica.

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