Griba
In today's world, Griba is a topic that is becoming more and more relevant. Whether in the personal, professional or social sphere, Griba is present in one way or another in people's daily lives. As technology advances and society evolves, Griba becomes a point of interest to better understand the world around us. In this article we will explore different aspects related to Griba, analyzing its impact in various areas and offering a broader perspective on this topic that is so recurrent today.
| Griba | |
|---|---|
 Maja e Këndrevicës seem from Vjosa valley | |
| Highest point | |
| Elevation | 2,122 m (6,962 ft) |
| Prominence | 1,662 m (5,453 ft) |
| Isolation | 77.4 km (48.1 mi) |
| Listing | Ultra, Ribu |
| Coordinates | 40°17′11″N 19°50′59″E / 40.286424°N 19.849716°E |
| Geography | |
  Griba | |
| Country |  Albania |
| Region | Southern Mountain Region |
| Municipality | Tepelenë |
| Geology | |
| Rock age(s) | Mesozoic, Paleogene |
| Mountain type | massif |
| Rock type(s) | limestone, flysch |
Griba is a massif situated in the Upper Kurvelesh region, within the boundaries of Tepelenë municipality, in southern Albania. Its highest peak, Maja e Këndrevicës, reaches a height of 2,122 m (6,962 ft).
Other high peaks include Maja e Tartarit 1,971 m (6,467 ft), Maja e Kulthit 1,907 m (6,257 ft), Maja e Sorrës 1,857 m (6,093 ft), Maja e Lopsit 1,837 m (6,027 ft), etc.[1]
Geology
The massif features a cone-shaped body with steep inclines and a flat peak and is composed primarily of Mesozoic and Paleogene limestones, with lesser amounts of flysch, giving it an asymmetrical anticlinal structure. Its ridge is marked by numerous karst pits and evidence of quaternary glaciations can be seen with the presence of cirques and moraines.[2]
Biodiversity
Vegetation is sparse but there are plenty of summer pastures and a variety of medicinal plants. In Dhëmblan, the laurel forest has been designated a protected nature reserve. The area is home to a thriving population of quail.