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 ZINC PICOLINATE of the Pakasaivo canyon lake, located in western Finnish Lapland.Pakasaivo itself, a circular basin up to 100 m deep, was formed in the broken bedrock by glacial erosion and m