Arnavutluk’un batısı, kuzeyden güneye kadar komple Adriyatik’e ve İyon Denizi’ne bakıyor. Kıyı böylesine uzun olunca doğal olarak bir uçtan öbürüne oldukça farklılık gösterebiliyor. Arnavutluk’un kuzeyinden ortalarına kadar uzanan kıyılar genellikle ince kum plajlardan oluşur. Bu yapı aslında Güney Karadağ sahillerinin devamı niteliğindedir ve güneye göre çok daha kalabalık olur. Güney sahilleri ise kuzeydeki sahilin aksine sert yamaçların eteklerinde bulunduğundan genellikle taşlık plajlardan oluşur. Bu durum tabii denizin rengine doğrudan etki ederek bu koy ve plajları oldukça çekici kılıyor.
The western part of Albania, from north to south, looks at the complex Adriatic and the Ionian Sea. When the coast is so long, it can naturally vary from one end to the other. The coasts that stretch from northern Albania to the center are usually made up of fine sand beaches. This structure is in fact a continuation of the Southern Montenegrin coast and is much more crowded than the south. The southern coasts, on the other hand, consist of stony beaches, as they are located on the slopes of the steep slopes, unlike the north coast. This, of course, makes the coves and beaches quite attractive by directly influencing the color of the sea.
The western part of Albania, from north to south, looks at the complex Adriatic and the Ionian Sea. When the coast is so long, it can naturally vary from one end to the other. The coasts that stretch from northern Albania to the center are usually made up of fine sand beaches. This structure is in fact a continuation of the Southern Montenegrin coast and is much more crowded than the south. The southern coasts, on the other hand, consist of stony beaches, as they are located on the slopes of the steep slopes, unlike the north coast. This, of course, makes the coves and beaches quite attractive by directly influencing the color of the sea.
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