Geology
The massif is composed entirely of a carbonate structure, with its surrounding slopes representing the plains of tectonic faults, cutting into the nearby valleys. The highest peak, Maja e Kollatës, stands at 2,553 meters tall and features a triangular shape, with a nearly flat surface called Podi i Kollatës, made up of flaky formations that are remnants of the Neogene era. After breaking at the tectonic-erosion pass of Rrethi i Bardhë, it continues to Maja e Thatë where it makes a sharp sudden turn from the northwest, breaking again at Qafa e Rupes , finally culminating at the border peak of Maja e Rosit . The western slope, wedged between Maja e Thatë and Maja e Rosit, has been shaped by intense frost activity, resulting in a relatively gentle relief called Pllana e Kukajt, which gradually descends into the glacial valley of Kukaj. The eastern slope is more fragmented, mainly due to its positioning at the forefront of the overpass. Here, where the cirques of the northeastern and eastern slopes end, two glacial-karst pits form, Mijusha and Lugu i Madh, both hanging over the Cerem basin. The peak section of the massif between Kollata and Maja e Rosit is divided by three trough (geology), troughs which have been shaped by glacial activity and formed along normal tectonic faults. The troughs of Perslopi and Vijat e Ujit flaunt in an almost parallel orientation between them (northeast-southwest), while the trough of Qafa e Rupes runs transversely.Biodiversity
The rugged terrain offers limited vegetation cover. A narrow beech belt grows at heights of . As the altitude increases, the landscape transitions to alpine pastures, filling the higher reaches of the massif.See also
* List of mountains in AlbaniaReferences
{{reflist Mountains of Albania Mountains of Montenegro Two-thousanders of Albania International mountains of Europe