description Nybroåsen Overview
Nybroåsen is an esker system in Kalmar County, in the Småland region of southeastern Sweden. It consists of ridges of sand and gravel deposited by meltwater beneath or within glacial ice during the Quaternary period. Because these permeable materials store and transmit groundwater, Nybroåsen is important as a groundwater reservoir around Nybro and has significance for local water supply and hydrogeology.
help Nybroåsen FAQ
What is Nybroåsen?
Nybroåsen is an esker system in Kalmar County in the Småland region of southeastern Sweden. It consists of sand and gravel ridges formed by meltwater connected with Quaternary glaciation.
How did the Nybroåsen ridges form?
Meltwater flowing beneath or within glacial ice deposited sand and gravel in long ridges. Those deposits remained as an esker system after the ice disappeared.
Why is Nybroåsen important for groundwater?
Its permeable sand and gravel can store and transmit groundwater. That makes an esker useful not only as a geological landform but also as part of the region's groundwater system.
Where in Sweden is Nybroåsen located?
It is in Kalmar County, within Småland in southeastern Sweden. The name refers to an esker system rather than a single mountain or town.
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