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Mavrovo Lake

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Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
Mavrovo Lake
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Mavrovo, Republic of Macedonia

Mavrovo Lake is situated in the Mavrovo region, in the Mavrovo and Rostuša municipality of the Republic of Macedonia, less than 100 km from Skopje. Abundant with trout, Lake Mavrovo is used for recreational activities such as swimming, boating and fishing during the summer. An additional point of interest is the half-submerged church in the lake. Spreading over an area of about 780 square kilometres , the Mavrovo National Park features deep canyons, snowy peaks and blue lakes combine with dense forests that abound with diverse wildlife. Mavrovo is one of the leading tourist areas in the country along with Ohrid, Prespa, Dojran, Popova Shapka , Pelister, and Kruševo. It was established in 1949 by a law passed by the National Assembly of Macedonia. Later the legislation was changed considerably, enforcing a much stricter protection system. According to the new law, the park is divided into three zones: strict nature reserves, managed reserves, and a tourist zone. One of the appealing features of Mavrovo National Park is its vivid topography. The relief of the park contains three Alpine mountain systems: the Šar, Korab and Bistra mountains. They are exceptionally high, the Šar and Korab, reaching heights of more than 2700 m . These tremendous mountains are distinguished by chains of snowy, jagged peaks and broad grassy plateaus below them. Between the three mountains extends the Radika gorge. More than 25 kilometres long. Vertical cliffs higher than 300 metres rise above the waters of the Radika river. In addition, the park area contains many other interesting natural phenomena—the highest waterfall in the Balkans , alpine bogs in the Šar mountains as remnants of the Ice age, rare karst relief in the Bistra mountains, as well as numerous glacial lakes throughout the Alpine zone.
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