description Linköpingsåsen Overview
Linköpingsåsen is an esker in and around Linköping, Sweden, formed when meltwater deposited layers of sand and gravel beneath the last continental ice sheet. The ridge is part of the glacial landscape of Östergötland and is visible within the modern Linköping area. As an urban esker, it is relevant to local geography, ground conditions, regional geology, and landscape planning.
help Linköpingsåsen FAQ
What is Linköpingsåsen?
Linköpingsåsen is an esker in and around Linköping, Sweden. An esker is a long ridge of sand and gravel deposited by meltwater beneath a continental ice sheet.
How did Linköpingsåsen form?
Meltwater flowing beneath the last continental ice sheet carried and deposited layers of sand and gravel. When the ice disappeared, the sediment remained as a raised ridge.
Where can Linköpingsåsen be seen?
The ridge is visible within the modern Linköping area in Östergötland. It is therefore both a glacial landform and part of the urban landscape.
What type of glacial landform is Linköpingsåsen?
It is an esker, a sinuous ridge made mainly from water-laid sand and gravel. Eskers differ from many moraine ridges because they form in meltwater channels beneath or within glacial ice.
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