Abstract
Separate regions within the Transantarctic Mountains, the uplifted flank of the West Antarctic rift system, appear to have distinct Neogene histories of glaciation and valley downcutting. Incision of deep glacial outlet valleys occurred at different times throughout central and northern Victoria Land. This is corroborated by measurements of cosmogenic nuclides
| Original language | English |
|---|---|
| Pages (from-to) | 145-172 |
| Journal | Global and Planetary Change |
| Volume | 23 |
| DOIs | |
| Publication status | Published - 1999 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 14 Life Below Water
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