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The Vršac Mountains ((セルビア語:Вршачке планине / Vršačke planine), Romanian:'' Munții Vârșeț''), also known as Vršac Hill ((セルビア語:Вршачки брег / Vršački breg), Romanian: ''Dealurile Vârșețului''), are mountains located near Vršac, in the Banat, Serbia and partially also in Romania. They represent an independent and distinct massif, 19 kilometers long and spreading on an area of 170 square kilometers, of which 122 belong to Serbia and 48 to Romania. The Vršac mountains have a shape of an arch, where the basic mountain mass takes the central position, while the hills extend to the south and north. The Mountains are built of Paleozoic rocks (which date back over 260 million years) which are surrounded by Neogene sediments (about 60 m.y.old), including those of the ancient Pannonian sea (about 25 m.y.old). Contrary to some literature data, the Vršac Mountains are not part of the Carpathians but belong to Serbian-Macedonian Massif according to their geotectonic position and geological structure. Specific forms of geomorphological diversity, naturally sculpted – made of gneiss and schist are represented in solitary or clustered hummocks. ==Peaks== In respect to the appearance of the Vršac mountains, four distinct shapes are clearly visible: *The Gudurica peak (Gudurički vrh), is the highest peak in Vojvodina, with its 641m above the sea level *The Tower of Vršac (Vršačka kula) - 399m *The Fox Head (Lisičija glava) - with its three peaks: * *The Vršac Peak (Vršački vrh) - 590m * *Lower Vršišor (Donji Vršišor) - 463m and Gudurica peak - 641m Between them there are vast rifts. Turska glava (402m), Đakov vrh (449m), and Kamenarica are also interesting places for climbers. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Vršac Mountains」の詳細全文を読む スポンサード リンク
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