evidence: Tuzla Island (Ukrainian: Тузла, Russian: Тузла, Crimean Tatar: Tuzla; from Turkic "tuzla" – salty, saline, literally: saltpan) is a sandy islet in the form of a spit located in the middle of the Strait of Kerch, between the Kerch Peninsula in the west and the Taman Peninsula in the east. The island was formed from part of the Taman Peninsula after a 1925 storm. Tuzla Island was formed when the spit that continued the Taman peninsula suffered from massive erosion during a major storm in 1925.[2] In ancient times (2,500 years ago) the sea level was four meters below the present, which meant that at the site of modern Tuzla was quite an extensive area of land, which was part of the Taman Peninsula. Taman Peninsula itself at that time was part of the Kuban delta, and was separated from the rest of the land by river channels, which drained into the Sea of Azov and the Black Sea. Some historians identify Tuzla as the island of Alopeka, mentioned by ancient authors, located in the waters of Cimmerian Bosporus, and when the island periodically joined to the Asian shore of the Bosporus, the resulting braid[clarification needed] was used as the entrance to the passage through the narrowest part of the Cimmerian Bosporus, which is located between Alopekoy and the European shore of the Bosporus. Other historians and geologists reject such a hypothesis, believing that neither the island nor the Tuzla Spit existed in ancient times.