description Högsbyåsen Overview
Högsbyåsen is a glaciofluvial esker in Kalmar County, Sweden, formed from sand and gravel deposited by meltwater beneath or near a former ice sheet. Its permeable sediments allow water to move through the ridge and contribute to local groundwater storage and flow. The formation is therefore relevant both to Quaternary geology and to the study and management of water supplies in Småland.
help Högsbyåsen FAQ
What is Högsbyåsen made of?
Högsbyåsen is a glaciofluvial esker made from sand and gravel. Those sediments were deposited by meltwater beneath or near a former ice sheet.
Where is Högsbyåsen located?
Högsbyåsen is in Kalmar County, Sweden. It forms a ridge created by glacial meltwater processes rather than by ordinary river deposition alone.
Why is Högsbyåsen important for groundwater?
Its permeable sand and gravel allow water to move through the ridge. That makes Högsbyåsen contribute to local groundwater storage and groundwater flow.
How did Högsbyåsen form?
Meltwater flowing beneath or close to a former ice sheet deposited sand and gravel in a long ridge. This type of glaciofluvial ridge is called an esker.
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