The Peaks of the Balkans Trail. Rudolf Abraham

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      Krš Bogićevica, viewed from the pass above Dobërdol, on the border between Albania and Montenegro (Stage 4)

      The mountains through which the Peaks of the Balkans route passes form the border between Albania, Montenegro and Kosovo. They occupy an area south of the River Lim and north of the Black Drin, bordered to the west and east by Lake Skadar and the headwaters of the White Drin respectively.

      Collectively, these mountains are known by several names – Prokletije or Bjeshkët e Namuna, meaning the ‘accursed mountains’, in Montenegrin and Albanian respectively, or (the part lying in Albania) the Albanian Alps. In some places, you may see signs referring to them as the ‘blessed mountains’ – a nice attempt to challenge the negative connotations of the ‘accursed’ part of their name (and frankly, when you’re hiking through this astonishingly beautiful part of Europe, this does seem more appropriate). In any case, for convenience, we’ll refer to them as Prokletije here. Prokletije forms the south part of the Dinaric Alps, a chain of mountains stretching some 700km and running in a northwest to southeast direction from the Slovenian border through Croatia, Bosnia, Montenegro, Albania and Kosovo.

      The Prokletije mountains are characterised by broad, glaciated valleys and steep-sided limestone peaks, particularly in the western half of the range in Albania and Montenegro – in Kosovo, the eastern half of the range has a more gentle profile. They include the highest peak in Montenegro (Maja Kolata, 2528m) and the highest peak in Kosovo (Gjeravica, 2656m), as well as the highest mountain in the Dinaric Alps, Maja Jezerces (2694m) in Albania (the highest mountain in Albania is Korab, 2764m, which lies further southeast on the border with Macedonia). All three of these can be climbed with only slight detours from the Peaks of the Balkans Trail, as can several other prominent peaks.

      The Prokletije mountains were formed some 100 million years ago, during the same period and process as the Alps – through the buckling and uplifting/folding of the Eurasian plate with the African plate, and the uplifting of the what had once been the bed of a shallow, tropical sea, where shells and other marine life had been deposited in layers over millions of years. The area is heavily glaciated (although no glaciers remain here today), and glaciation occurred at a lower altitude than in the Alps further north – Lake Plav is the largest glacial lake in the Balkans, and a glacier in the Plav/Gusinje area is thought to have been around 35km long and up to 200m thick.

      Karst features – distinctive fluting, pans, sinkholes and limestone pavement formed by the gradual dissolving of limestone rock by rainwater – are prominent in Prokletije, particularly in the western half of the range. However, unlike most other popular hiking areas in the karst mountains of Montenegro (and neighbouring Croatia), availability of surface water is good on the Peaks of the Balkans Trail, with fairly abundant springs and mountain streams.