description Österfärneboåsen Overview
Österfärneboåsen is an esker in Sweden, a glacial ridge formed from material deposited by meltwater. It is identified as the western branch of Enköpingsåsen north of Tärnsjö and belongs to a large glacial deposit in the Swedish landscape. The feature is relevant to readers interested in Swedish geography, glacial landforms, and the physical traces left by Ice Age processes in the landscape.
help Österfärneboåsen FAQ
What is Österfärneboåsen?
Österfärneboåsen is an esker in Sweden. An esker is a glacial ridge made from sediment deposited by meltwater beneath or within a glacier.
Where is Österfärneboåsen located?
It lies north of Tärnsjö in Sweden. It is identified as the western branch of Enköpingsåsen.
How was Österfärneboåsen formed?
The ridge formed from material carried and deposited by glacial meltwater. Its long, narrow landform reflects the channel through which the meltwater moved.
Is Österfärneboåsen part of a larger glacial landscape?
Yes. Österfärneboåsen belongs to a large glacial deposit in the Swedish landscape and is connected with the Enköpingsåsen system.
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