Jezerca Peak (Albanian: Maja Jezercë) is the highest peak in the Dinaric Alps, the fifth highest in Albania and the sixth highest in the Balkans, standing at 2,694m (8,839ft) above sea level. It is the 28th most prominent mountain peak in Europe, and is regarded as one of the toughest and most dangerous climbs in the Albanian Alps.[3]
Maja Jezercë is situated within the Accursed Mountains range, which is noted for several small glaciers - among the southernmost glacial masses in Europe[4] after Snezhnika glacier (latitude of 41°46′09″ N)[5][6] and Banski Suhodol Glacier in Pirin mountain in Bulgaria. Apart from certain areas north of the peak, the limestone mountain massif is part of the National Parks of Theth and Valbonë Valley.[7] It can be climbed from the north; most climbers come from Gusinje in Montenegro as well as from Theth.[8]
The summit is 5km (3mi) from the border with Montenegro, between the Valleys of Valbonë to the east and the Shala to the west. In part, the whole floor between the valley of Valbonë, Shala, Ropojana and Maja Roshit2,522m (8,274ft) is known as Jezercë, in addition to the peak, Jezercës borders other peaks such as the Maja e Popljuces (2,569 metres (8,428ft)) and the Maja e Alisë2,471m (8,107ft) in the west, Maja Rrogamit2,478m (8,130ft) to the east, Maja Kolajet2,498m (8,196ft), Maja Malësores 2,490m (8,169ft), Maja Bojs2,461m (8,074ft) in the northwest,
Maja Kokervhake2,508m (8,228ft) and Maja Etheve2,393m (7,851ft) in the north.
Name
Having been invaded by Serbs from the Ottomans in 1913 and annexed by the Kingdom of Serbia prior to the Treaty of London and the creation of the first Albanian state in that same year, the name is etymologically derived from the Serb word for lake: "Jezero".[9][10][11][12] Jezerski Vrh means "lake peak". The toponym refers to the cirque lakes in the lower part of the Buni i Jezercës on the northern side of the mountain. During the Titoist era it was given the name of Maja e Rinisë (Mountain of Youth), which never stuck.[8]
Topology
Jezerca is a large rocky peak of dolomitic limestone. There is almost no vegetation there. North, east and west of the mountain top is in great cirque from that in the glacial periods when glaciers were more extensive than today. Today the northern cirque is called Buni i Jezercës at a height of 1,980 metres (6,500ft) and 2,100 metres (6,900ft) in height around 400 metres (1,300ft). Because it is located in the wettest region of Europe with around 6 metres (240in) of rainfall[dubious– discuss] equivalent believed to fall on the western slopes, snowfall is so great that only in dry years do even the less exposed sections melt away.[13]
Gallery
The summit seen from the top of Karanfili 2,480m (8,136ft).
Kolcakovski, Belj (1997). The periglacial zone of high mountains of Serbia and Macedonia and its basic characteristics. Observatoire de Montagne de Moussala.
Milivojević, Milovan; Menković, Ljubomir; Ćalić, Jelena (2008), "Pleistocene glacial relief of the central part of Mt. Prokletije (Albanian Alps)", Quaternary International, 190: 112–122, doi:10.1016/j.quaint.2008.04.006
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