MONTENEGRO: Durmitor National Park

Received thanx to Ana.


The Black Lake(Crno Jezero)

Durmitor National Park comprises Mount Durmitor plateau and the valley formed by the canyon of the River Tara, incorporating three major geomorphologic features: canyons, mountains and plateaux. Because of its geographical location and range in altitude, the park is under the influence of both Mediterranean and alpine microclimates, which has resulted in an exceptional range of species.

Geologically, Durmitor and Tara canyons are made up of rocky massifs of the Mesozoic era (from the Lower Triassic to the Upper Cretaceous), Tertiary and Quaternary periods. The dominant features are the limestone formations of the Middle and Upper Triassic, the Upper Jurassic and the Upper Cretaceous, especially the so-called Durmitorean flysch. The River Tara, one of the last wild rivers in Europe, has pure, clear waters, a gorge 1,300 m deep and notable floristic and faunistic diversity. The 16 glacial lakes of the Durmitor and the canyons of the Tara, Susica and Draga rivers were formed during the Quaternary period, following the sudden thaw of the snow and the formation of glaciers on the Durmitor and neighbouring mountains. The waters of the largest lake, Black Lake, feed two separate river basins: the River Tara, and underground through the Durmitor Massif, the River Komarnica or Piva. There are numerous examples of weathering processes, rock shapes and land features characteristic of karstic erosion, fluvial erosion and glacial erosion.

Vegetation zones include deciduous forest, coniferous forest and subalpine zones. The dominant species include Scots pine, Norway pine, silver fir, beech, occasional birch, mugo pine and juniper. The park supports a rich karstic flora with many rare and endemic species. There are 37 taxa endemic to the area and six specific to Durmitor. The park contains one of the last virgin black pine forests in Europe, on soils that would usually develop beech woodland.

The Tara and its tributaries, as well as the lakes, contain a large number of salmonidae. Forest fauna includes brown bear, wolf, wild boar, wild cat, chamois, various species of eagle, capercaillie, black grouse and rock partridge.

MONTENEGRO: Natural and Culturo-Historical Region of Kotor

Received thanx to Ana from Macedonia.
Kotor Starigrad.

The culturo-historical region of Kotor has exerted considerable influence, over a span of time and within a cultural area of the world, on developments in architecture and human settlement. Kotor and its neighbours were main bridgeheads of Venice on the southern Adriatic coast. Its art, goldsmithing and architecture schools had a profound and durable influence on the arts of the coast. It is among the most characteristic examples of a type of structure representing important cultural, social and artistic values. It is considered to possess outstanding universal value by the quality of its architecture, the successful integration of its cities to the Gulf of Kotor and by its unique testimony to the exceptionally important role that it played in the diffusion of Mediterranean culture in the Balkan lands.

Founded by the Romans on the Adriatic coast in Montenegro, Kotor developed in the Middle Ages into an important commercial and artistic centre with its own famous schools of masonry and iconography. Throughout the centuries, many empires battled for control of the city. In the 10th century, it was an autonomous city of the Byzantine Empire. From 1186 to 1371, it was a free city of medieval Serbia. It was under Venetian and Hungarian control for brief periods, an independent republic from 1395 to 1420, and then returned to Venetian control once again. French occupation from 1807 to 1914 was followed by Austrian rule until 1918, when Kotor finally became part of Yugoslavia. Throughout its turbulent history, a variety of buildings have been erected. The largest and most impressive of these is the St Tryphon Cathedral. The original church was constructed in the 8th century, according to the annals of the Byzantine Emperor. A new church, built in 1166, was subsequently damaged during the 1667 earthquake and then restored.

The limits of the World Heritage site coincide approximately with the crests of the natural sinkhole formation. At both ends, the site is bordered by the national parks of Orten and Lovcen, making a vast protected natural area. The Gulf of Tivat (formerly part of the approaches to Kotor) is omitted because of the authenticity of its settlements, which has been downgraded by recent industrialization (shipyards, harbour equipment).

Most of Kotor's palaces and houses, many Romanesque churches, all of Dobrota's palaces, and Perast's main buildings have all suffered from earthquakes, and some have been partly destroyed. The city was evacuated by all its inhabitants after the most recent, on 15 April 1979. An intensive restoration and reconstruction programme has now been completed and the city is flourishing again.