description Epilänharju Overview
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Where is Epilänharju located?
Epilänharju is an esker ridge in Vaasa, Finland. It is recognized as a geological remnant from the last glacial period.
How did Epilänharju form?
Epilänharju formed from sediments carried by meltwater beneath or within glacial ice. As the ice retreated, the sand and gravel remained as a raised ridge.
Why is Epilänharju important in Vaasa?
The ridge is a visible record of the glacial processes that shaped the Vaasa region. Its landform preserves evidence from the last Ice Age in the Finnish landscape.
What is an esker ridge?
An esker ridge is a long, narrow deposit of sand and gravel left by glacial meltwater. Epilänharju is a local Finnish example of this landform.
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