Moraines and dead ice in Taylor Valley, Antarctica, record retreat of alpine and outlet glaciers from Marine Isotope Stage 5 to 4
Debris-covered glaciers and dead ice are common in the Transantarctic Mountains. We investigated the origin and structure of a 0.1 km2 buried dead ice mass in Taylor Valley near the terminus of Taylor Glacier, an outlet from the East Antarctic Ice Sheet. The dead ice occupies a lobate landform on th...
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| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis Group
2025-12-01
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| Series: | Arctic, Antarctic, and Alpine Research |
| Subjects: | |
| Online Access: | https://www.tandfonline.com/doi/10.1080/15230430.2025.2478696 |
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