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...

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Bibliographic Details
Main Authors: Rempel, Alan, Meyer, Colin, Robel, Alexander
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2021
Subjects:
Heinrich event
Frozen Fringe
Laurentide
Hudson
Hudson Strait
Ice Shelf
North Atlantic
Online Access:https://dx.doi.org/10.18739/a2bz6190n
https://arcticdata.io/catalog/view/doi:10.18739/A2BZ6190N

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