Eskers and bedrock gorges (tunnel valleys) in the Pakasaivo area, western Finnish Lapland

Studies of the deglaciation of the last Scandinavian Ice Sheet, including the behavior of the ice sheet and meltwater activity, were conducted in the vicinity of the Pakasaivo canyon lake, located in western Finnish Lapland. Pakasaivo itself, a circular basin up to 100 m deep, was formed in the brok...

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Bibliographic Details
Published in:Bulletin of the Geological Society of Finland
Main Author: P. Johansson
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of Finland 2003
Subjects:
glacial geology
deglaciation
subglacial environment
eskers
meltwater channels
canyons
lakes
erosion
Pakasaivo
Lapland Province
Finland
Geology
QE1-996.5
Canyon Lake
Dammed Lake
Ice Sheet
Lapland
Online Access:https://doi.org/10.17741/bgsf/75.1-2.001
https://doaj.org/article/aa79faa56bdf4bf38f9de9b07b1519f1

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