description Køge Ås Overview
Køge Ås represents a significant glacial landform within the Køge area of Denmark. This esker system, formed during the last Ice Age, showcases a distinctive tunnel valley carved by ancient meltwater flows. The site’s notable geological features provide valuable insights into Zealand's glacial history and are of interest to geologists, archaeologists, and those studying Danish landscape evolution.
help Køge Ås FAQ
How was Køge Ås formed?
Køge Ås consists largely of gravel deposited by a meltwater river flowing beneath the ice that covered Zealand. When the ice disappeared, those subglacial deposits remained as a long, narrow ridge called an esker.
How long is the Køge Ås ridge?
The Geological Survey of Denmark and Greenland describes a ridge running roughly 20 kilometers west from Køge toward Haraldsted Lake. Some local descriptions treat the wider chain of surviving hills as approximately 35 kilometers long.
Can visitors walk along Køge Ås?
Yes, the Køge Å trail provides a walking and cycling route of about 22 kilometers between the Køge area and Borup. Access varies because parts of the ridge cross privately owned land and former gravel-extraction areas.
Why are sections of Køge Ås missing?
The ridge contains commercially useful sand and gravel, so quarrying removed or interrupted portions of the original landform. The remaining sections still expose evidence of meltwater deposition during the last Ice Age.
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