description Uppsalaåsen Overview
Uppsalaåsen is a major glacial esker in central Sweden and an important landscape feature of Uppsala County. It was formed from sand and gravel deposited by meltwater flowing through or beneath the Scandinavian ice sheet during its retreat. The ridge provided elevated, relatively well-drained ground on which parts of Uppsala developed, and its permeable deposits also make eskers important sources and storage areas for groundwater.
help Uppsalaåsen FAQ
What is Uppsalaåsen?
Uppsalaåsen is a major glacial esker in central Sweden and an important landscape feature of Uppsala County. It is a long ridge made mainly from sand and gravel deposited by glacial meltwater.
How was Uppsalaåsen formed?
Meltwater flowing through or beneath the Scandinavian ice sheet deposited sand and gravel as the ice retreated. When the ice disappeared, those deposits remained as the raised ridge known as an esker.
Where is Uppsalaåsen located?
It runs through central Sweden and is closely associated with Uppsala County. Its elevated route has influenced settlement, transport, and access to parts of the surrounding landscape.
What is an esker?
An esker is a ridge formed by sediment deposited by meltwater beneath or within a glacier. Uppsalaåsen is a Swedish example created during the retreat of the Scandinavian ice sheet.
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