Substantial spatial variation in glacial erosion rates in the Dronning Maud Land Mountains, East Antarctica
The topography of the Dronning Maud Land Mountains, Antarctica, has become more pronounced and rugged since preglacial times due to higher glacial erosion at low elevations and lower erosion at high elevations, according to low-temperature thermochronology
Published in: | Communications Earth & Environment |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Portfolio
2021
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Subjects: | |
Online Access: | https://doi.org/10.1038/s43247-021-00315-3 https://doaj.org/article/6cc0267b0b1a44a790e3055b6f52f6e6 |
Summary: | The topography of the Dronning Maud Land Mountains, Antarctica, has become more pronounced and rugged since preglacial times due to higher glacial erosion at low elevations and lower erosion at high elevations, according to low-temperature thermochronology |
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