Pannonian Sea
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The Pannonian Sea (also known as Paratetis) was a shallow ancient sea located in the area today known as the Pannonian Plain in Central Europe. The Pannonian Sea reached its greatest extent during the Pliocene, when three to four kilometres of sediments were deposited.
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[edit] History
Pannonian Sea was formed in the end of the Oligocene and beginning of the Miocene Epoch. Pannonian Sea was connected with another prehistoric sea known as Tetis (two seas were connected through the territoty of modern Rona Gulf, Bavaria and Vienna Basin). During the Miocene Epoch, the connection between two seas was interrupted.
Through the Đerdap Strait, Pannonian Sea was connected to another sea located in Wallachian-Pontic Basin. During its largest sea level, Pannonian Sea reached the south of modern Serbia (a gulf of the Pannonian Sea located in modern Morava river valley stretched to modern Grdelica Gulch and Vranje Depression and was connected to the Aegean Sea through the modern Preševo Valley).
Pannonian Sea existed about 30 million years. It disappered in the middle of Pleistocene Epoch, about 600,000 years ago. The water of the Pannonian Sea actually ruptured its way through the modern Đerdap Gorge on the Danube river and flowed through the gorge lefting behind a large plain known as the Pannonian Plain. The remnants of the former islands of the Pannonian Sea are modern Pannonian Island Mountains (Fruška Gora and Vršac Mountains).
[edit] Pannonian Sea in modern culture
Pannonian Sea was a subject of the popular song "Panonski mornar" ("Pannonian sailor") of the Serbian singer Đorđe Balašević. [1]
[edit] References
- Dragan Rodić, Geografija za I ili III razred srednje škole, Zavod za udžbenike i nastavna sredstva, Beograd, 1995.
