Articles | Volume 4, issue 4
https://doi.org/10.5194/esurf-4-831-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/esurf-4-831-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Reconstruction of North American drainage basins and river discharge since the Last Glacial Maximum
Department of Earth Sciences and Saint Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA
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- Organization and reorganization of drainage and sediment routing through time: the Mississippi River system M. Blum 10.1144/SP488-2018-166
- 10Be dating of former glacial Lake Naskaupi (Québec-Labrador) and timing of its discharges during the last deglaciation H. Dubé-Loubert et al. 10.1016/j.quascirev.2018.05.008
- Multiple meltwater discharge and ice rafting events recorded in the deglacial sediments along the Beaufort Margin, Arctic Ocean S. Klotsko et al. 10.1016/j.quascirev.2018.11.014
2 citations as recorded by crossref.
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Latest update: 14 Dec 2024
Short summary
The ice sheets that once spread across northern North America dramatically changed the drainage basin areas and discharges of rivers across the continent. As these ice sheets retreated, starting around 19 500 years ago, they sent meltwater to the oceans, influencing climate and building a geologic record of deglaciation. This record can be used to evaluate ice-sheet reconstructions and build an improved history and understanding of past ice-sheet collapse across North America.
The ice sheets that once spread across northern North America dramatically changed the drainage...
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