The Korçë Plain (Albanian: Fusha e Korçës) or Korça Basin is a small, fertile, intermountain basin in southeastern Albania.
In its southern side is found the Kamenica Tumulus.
The Korçë Plain (Albanian: Fusha e Korçës) or Korça Basin is a small, fertile, intermountain basin in southeastern Albania.
In its southern side is found the Kamenica Tumulus.
The Dassaretii (Ancient Greek: Δασσαρῆται, Δασσαρήτιοι, Dassaretai, Dassaretioi; Latin: Dassaretae, Dassaretii) were an Illyrian people that lived in the inlands of southern Illyria, between present-day south-eastern Albania and south-western North Macedonia. Their territory included the entire region between the rivers Asamus and Eordaicus (whose union forms the Apsus), the plateau of Korça locked by the fortress of Pelion and, towards the north it extended to Lake Lychnidus up to the Black Drin. They were directly in contact with the regions of Orestis and Lynkestis of Upper Macedonia. Their chief city was Lychnidos, located on the edge of the lake of the same name. One of the most important settlements in their territory was established at Selcë e Poshtme near the western shore of Lake Lychnidus, where the Illyrian Royal Tombs were built.
The Dassaretii were one of the most prominent peoples of southern Illyria, forming an ethnic state. They made up the ancient Illyrian kingdom that was established in this region. The weakening of the kingdom of the Enchelei presumably led to Enchelei's assimilation and inclusion into a newly established Illyrian realm at the latest in the 6th–5th centuries BC, marking the arising of the Dassaretii, who appear to have replaced the Enchelei in the lakeland area.
The Central Mountain Region (Albanian: Krahina Malore Qëndrore) is a physiogeographical region encompassing the central and eastern edge of Albania. It comprises the mountainous inland extending all the way from the valley of Drin and the mountains of Sharr, Skanderbeg, Korab, and Shebenik-Jabllanicë, through the lakes of Ohrid and Prespa, until it reaches the village of Ersekë and the mountains of Pindus close to the border between the country and Greece.
The central mountain range can be conventionally divided into a number of subregions. The north encompasses the mountainous districts of Mirditë and Pukë. The center is dominated by the mountains of Lurë and Korab alongside the regions of Martanesh and Çermenikë. The south includes the valley of Shkumbin as well as the mountains of Mokër and Valamara, the plain of Korçë with the upper districts of Devoll and Kolonjë.
The Devoll (Albanian: Devoll; Albanian definite form: Devolli) is a river in southern Albania.It is one of the source rivers of the Seman. It is 196 km (122 mi) long and its drainage basin is 3,130 km (1,210 sq mi). Its average discharge is 49.5 m/s (1,750 cu ft/s). Its source is in the southwestern corner of the Devoll municipality, close to the Greek border. It flows initially northeast, through Miras, then north through Bilisht, and northwest through Progër, Pojan (in the northern Korçë Plain which was marshy until after the World War II), Maliq, Moglicë, Kodovjat, Gramsh, where it is stowed in a big lake and Gostimë, where it turns south. It joins the Osum near Kuçovë, to form the Seman. The Seman opens into a small delta south of the Karavasta lagoon in the Adriatic Sea.
A number of hydroelectricity plants on the river Devoll are planned or under construction. The Albanian company Devoll Hydropower, owned and operated by the Norwegian power company Statkraft, is building two hydroelectricity plants near Banjë (Banjë Hydro Power Plant) and near Moglicë (Moglicë Hydro Power Plant), with combined capacity 242 MW. The decision whether a third plant near Kokel is to be built, will be taken when the first two dams are completed.
Cangonj Pass (Albanian: Gryka e Cangonjit; Albanian pronunciation: [ɡɾyːka e t͡sanˈɡɔɲit]) is a mountain pass located in the village of Cangonj, Korçë County, southeastern Albania. It is located between Mount Moravë and Mount Ivan south of Lake Prespa, and connects the Korçë Plain in the west with the Poloskë-Bilisht plain in the east. Crossed by the Devoll, the mountain pass was formed through the millennia by the excavating process of the flow of this river.
In classical antiquity the name of the mountain pass was recorded as Tsangon, which was traditionally a border area between Macedon and Illyria, being part of an important east-west communication route.