Shkumbin in the context of "Shebenik"

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.

Taulantii or Taulantians ('swallow-men'; Ancient Greek: Ταυλάντιοι, Taulantioi or Χελιδόνιοι, Chelidonioi; Latin: Taulantii) were an Illyrian people that lived on the Adriatic coast of southern Illyria (modern Albania). They dominated at various times much of the plain between the rivers Drin (Drilon) and Vjosa (Aoös). Their central area was the hinterland of Epidamnos-Dyrrhachion, corresponding to present-day Tirana and the region between the valleys of Mat and Shkumbin (Genusus). The Taulantii are among the oldest attested Illyrian peoples, who established a powerful kingdom in southern Illyria. They are among the peoples who most marked Illyrian history, and thus found their place in the numerous works of historians in classical antiquity.

The Principality of Albania (Albanian: Principata e Arbërisë) was an Albanian principality ruled by the Albanian dynasty of Thopia. The first notable ruler was Tanusio Thopia, who became Count of Mat in 1328. The principality would reach its zenith during the rule of Karl Thopia, who emerged in 1359 after the Battle of Achelous, conquering the cities of Durrës and Krujë and consolidating his rule of central Albania between the rivers of Mat and Shkumbin. The principality would last up until 1415, when it was conquered by the Ottoman Empire.

Skanderbeg Mountains (Albanian: Vargmalet e Skënderbeut), also known as Vargmalet Perëndimore, are a prominent mountain range situated in the northwestern section of the Central Mountain Region of Albania. The range stretches approximately 100 km (62 mi), making it the longest in the country. It extends from the Gjadër river valley in the northwest to the Shkumbin river valley in the southeast; and from the trough of Mat in the east, to the plains between Lezhë, Tirana and Lower Shkodër in the west.

The eastern side of the range is composed primarily of limestone from the Triassic-Jurassic periods, separated into distinct blocks, while the western side is composed of limestone from the Ordovician and the Cretaceous-Paleogene periods, forming belts amid the Paleogene flysch. Ultrabasic rocks are also present, and the older flysch appears in the form of surface bands on the eastern side of the range.

The Via Egnatia was a road constructed by the Romans in the 2nd century BC. It crossed Illyricum, Macedonia, and Thracia, running through territory that is now part of modern Albania, North Macedonia, Greece, and European Turkey as a continuation of the Via Appia.

Starting at Dyrrachium (now Durrës) on the Adriatic Sea, the road followed a difficult route along the river Genusus (Shkumbin), over the Candaviae (Jablanica) mountains and thence to the highlands around Lake Ohrid. It then turned by parts south, following several high mountain passes to reach the northern coastline of the Aegean Sea at Thessalonica. From there it ran through Thrace to the city of Byzantium (later Constantinople, now Istanbul). It covered a total distance of about 1,120 km (696 miles/746 Roman miles). Like other major Roman roads, it was about six metres (19.6 ft) wide, paved with large polygonal stone slabs or covered with a hard layer of sand.

Selcë e Poshtme ("Lower Selcë") is a village located in the Mokra area, Korçë County, Albania. At the 2015 local government reform it became part of the municipality Pogradec. Near the village, on the right bank of Shkumbin river at an elevation of 1,040 metres (3,410 ft) above sea level, 5 Illyrian Royal Tombs of Selca e Poshtme are found. In 1996, Albania included the Royal Tombs of Lower Selcë in the UNESCO World heritage list of proposals.

The Illyrian Tombs of Selca e Poshtme (Albanian: Varret e Selcës së Poshtme) are located near the town of Pogradec in Albania near the village of Selcë e Poshtme. On the right bank of the river Shkumbin at an elevation of 1040 m above sea level, lie the remains of the ancient city of Pelion and the accompanying necropolis. The Roman Via Egnatia led past it towards Thessaloniki. Though there are traces of human activity in Neolithic times, the settlement proper dates to the Iron Age (Illyrian proto-urban) through to the Illyrian urban period (5th to 2nd centuries BC), and reached its height under settlement by the Illyrian tribe of Enchele in the later Iron Age and was also occupied in the Roman period as traces of a municipal building show. From the 4th to 1st centuries BC the city was the royal residence of Illyrian kings and therefore, also probably an important political and economic centre. In 1996, Albania included the Royal tombs of Selca e Poshtme in the UNESCO World heritage list of proposals.

Tosk (Albanian definite form: toskërishtja) is the southern group of dialects of the Albanian language, spoken by the ethnographic group known as Tosks. The line of demarcation between Tosk and Gheg (the northern variety) is the Shkumbin River. Tosk is the basis of the standard Albanian language.

Major Tosk-speaking groups include the Myzeqars of Myzeqe, Labs of Labëria, Chams of Çamëria, Arvanites of Greece and the Arbëreshë of Italy, as well as the original inhabitants of Mandritsa in Bulgaria. In North Macedonia, there were approximately 3000 speakers in the early 1980s.