Sediment freeze-on during Heinrich events; Laurentide; modeling study 2019
Anomalous coarse-grained sediment layers beneath the North Atlantic likely originated from sediment freeze-on to the base of ice sheets during the last glacial period. These layers represent periods of extreme ice discharge, called Heinrich events, and are variously attributed to ice stream flow ins...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
NSF Arctic Data Center
2021
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Subjects: | |
Online Access: | https://dx.doi.org/10.18739/a2sn0154f https://arcticdata.io/catalog/view/doi:10.18739/A2SN0154F |