During the peak of the last global glacial extent (c. 22,000 – 18,000 years ago), ice-sheets capped the W. Pindοs high altitude (> 2500m) summits and karst plateaus enhancing erosion of the limestone and flysch bedrock and discharging massive water volumes into the Vikos – Voidomatis – Aoos river system. Natural resources were then scarce […]
Hunters of the last Ice Age in the Voidomatis valley
![](https://vikosaoosgeopark.com/wp-content/uploads/2016/06/η-Βραχοσκεπή-Κλειδί-στο-φαράγγι-του-Βoϊδομάτη-ΧΠ-1200x602.jpg)