Butrint National Park in the context of "Ancient civilisation"

Butrint (Greek: Βουθρωτόν and Βουθρωτός, romanized: Bouthrōtón, Latin: Buthrōtum, Albanian: Butrint) was an ancient Greek polis and later Roman city and the seat of an early Christian bishopric in Epirus.

Originally a settlement of the Greek tribe of the Chaonians, it later became part of the state of Epirus and later a Roman colonia and a Byzantine bishopric. It entered into decline in Late Antiquity, before being abandoned during the Middle Ages after a major earthquake flooded most of the city. In modern times it is an archeological site in Vlorë County, Albania, some 14 kilometres (8.7 mi) south of Sarandë, close to the Greek border. It is located on a hill overlooking the Vivari Channel and is part of the Butrint National Park. Today, Bouthrotum is a Latin Catholic titular see and also features the Ali Pasha Castle.

Ksamil (Albanian: Ksamili; Greek: Εξαμίλι) is a village and a former municipality in the riviera of Southern Albania, and part of Butrint National Park. At the 2015 local government reform it became a subdivision of the municipality of Sarandë. The population as of the 2023 census is 2,731, while according to the Civil Offices it was 9,137 in 2018. The municipal unit consists of the villages Ksamil and Manastir. During the communist era, the coastal village of Ksamil was built in 1966 and is located south of Sarandë off the road to Butrint.

The Islets of Ksamil (Albanian: Ishujt e Ksamilit or Ishujt e Tetranisit), consist of four rocky islets located in the direct proximity to the Ionian Sea in Southern Albania. The village of Ksamil, after whom the islets are named, is located to the east of the islets. Furthermore, the islands are situated within the boundaries of the Butrint National Park.

The islets lie to the extreme south of the Albanian Riviera along the Ionian Sea. They are remote and can only be accessed by boat. The combined areas of the four islands is only 8.9 hectares (22.0 acres). The two outer islands are connected by a narrow strip of sand. In terms of geology, the islands have been shaped into its current form over the Jurassic period, with its disjunction of the mainland due to the water activity.