Geography
Lake Ohrid is the deepest lake of the Balkans, with a maximum depth of 288 m (940 ft) and a mean depth of 155 m (508 ft). It covers an area of 358 km² (138 sq mi), containing an estimated 55.4 km³ of water. It is 30.4 km long by 14.8 km wide at its maximum extent with a shoreline length of 87.53 km, shared betweenMacedonia (56.02 km) and Albania (31.51 km). The Ohrid Lake is divided between Republic of Macedonia and Albania. Of the total surface area, 248 km2 belongs to Republic of Macedonia and 110 km2 belongs toAlbania
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Origin
The Ohrid and Prespa Lakes belong to a group of Dessaret basins that originated from a geotectonicdepression during the Pliocene epoch up to five million years ago[3] on the western side of the Dinaric Alps. Worldwide, there are only a few lakes with similarly remote origins with Lake Baikal and Lake Tanganyikabeing the most famous. Most other, short-lived lakes have a life span of less than 100,000 years before they are eventually filled up with sediments. It is believed that in the case of Lake Ohrid this process was delayed by its great depth and small sediment input from its filtered spring inflows. Moreover the Ohrid-Korca graben to the south of the lake is still tectonically active and might compensate sedimentation by subduction. In contrast to Lake Ohrid, Lake Prespa is likely to have turned dry several times in its history, as a result of its karstic underground.[4] In 2008, Macedonian media reported that international experts will be researching the lake in order to determine its age.[5]
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