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===The lake=== Skanderborg Sø (English: ''Skanderborg Lake'') was created during the [[Weichselian glaciation|last ice age]] and formed from a melting block of ice left behind; a so-called [[kettle hole]]. The lake has an irregular shape divided into two larger lake-areas known as Hylke and Store Sø respectively, with a total surface area of 8.6 square kilometers. The lake has an average depth of 8 meters and up to 18.8 meters at the deepest spot. It holds approximately 49.3 million cubic meters of freshwater 23.5 meters above sea level<ref name=DAFC/><ref>[http://mossoen.dk/User_files/1ece7ca54a5ef93326d1e0f22a31f493.pdf Mossø and surrounding lakes] {{webarchive|url=https://web.archive.org/web/20140222135834/http://mossoen.dk/User_files/1ece7ca54a5ef93326d1e0f22a31f493.pdf |date=22 February 2014 }} [[National Survey and Cadastre of Denmark]] (KMS) 2012. Basic numbers. {{in lang|da}}</ref> and empties into [[Mossø]], by the short stream of Tåning Å in the west. There are a number of small isles in the lake; Kalvø, Æbelø, Sct. Thomas and Sct. Helene.<ref>[http://www.skanderborgleksikon.dk/index.php/Sct._Helene Sct. Helene] Skanderborg Leksikon {{in lang|da}}</ref>
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