The rolling hills of the moraine landscape north of the Main Stationary Line of the Ice was formed during Weichsel 22-20.000 years ago. The landscape is cut by many meltwater valleys that are not suitable for modern agriculture. They are often used for grazing or covered by trees and with water courses in the bottom. The natural value of these areas is often very high.
#kabbel #tannebaek valley #moraine landscape #nature #grazing #geosite
Taget | 2016-05-17 |
Uploaded | for 3 år siden |
Opløsning | 3264 x 2448 px |
Størrelse | 3.32 MB |
Copyright | Geopark Vestjylland |
Mime Type | image/jpeg |