Dinaric Alps

Dinaric Alps
Dinarides
Orjen at the Bay of Kotor is the most heavily karstified range of the Dinarides
Highest point
Peak	Maja Jezercë (Albania)
Elevation
Coordinates
Dimensions
Length	NW-SE
Geography
Topography of the Dinaric Alps Topography of the Dinaric Alps
Countries	List Albania Bosnia and Herzegovina Croatia Kosovo Montenegro Serbia Slovenia
Borders on	Julian Alps
Geology
Age of rock	Mesozoic Era
Type of rock	Sedimentary

The Dinaric Alps or Dinarides is a mountain chain which spans areas of Albania, Bosnia and Herzegovina, Croatia, Kosovo, Montenegro, Serbia and Slovenia.

They extend for 645 kilometres (401 mi) along the coast of the Adriatic Sea (northwest-southeast), from the Julian Alps in the northwest down to the Šar-Korab massif, where the mountain direction changes to north-south. The highest mountain of the Dinaric Alps is Mount Prokletije, located on the border of eastern Montenegro and northern Albania, with the peak called "Lake Crest" at 2,694 metres (8,839 ft).

The Dinaric Alps are the fifth most rugged and extensively mountainous area of Europe after the Caucasus Mountains, Alps, Pyrenees and Scandinavian Mountains. They are formed largely of Mesozoic and Cenozoic sedimentary rocks of dolomite, limestone, sand and conglomerates formed by seas and lakes that had once covered the area. During the Alpine earth movements that occurred 50–100 million years ago, immense lateral pressures folded and overthrust the rocks in a great arc around the old rigid block of the northeast. The Dinaric Alps were thrown up in more or less parallel ranges, stretching like necklaces from the Julian Alps as far as the areas of northern Albania and Kosovo, where the mountainous terrain subsides to make way for the waters of Drin and the fields of Kosovo. The Šar and Korab mountains then rise and the mountainous terrain continues southwards to the Pindus of Greece and the mountains of the Peloponnese and Crete, Rhodes to the Taurus Mountains of southern Turkey.

Name

The Dinarides are named after Mount Dinara (1,913 m), a prominent peak in the center of the mountain range on the border of Croatia and Bosnia and Herzegovina. The chain is called Alpet Dinaride or Alpet Dinarike in Albanian, Dinarsko gorje or Dinaridi in Bosnian and Croatian, Dinarske planine or Динариди in Serbian and Dinarsko gorstvo in Slovene.

Geology

Valbona Pass, northern Albania

The Mesozoic limestone forms a very distinctive region of the Balkans, notable for features such as the Karst, which has given its name to all such terrains of limestone eroded by groundwater. The Quaternary ice ages had relatively little direct geologic influence on the Balkans. No permanent ice caps existed, and there is little evidence of extensive glaciation. Only the highest summits of Durmitor, Orjen and Prenj have glacial valleys and moraines as low as 600 m (1,969 ft). However, in the Prokletije, a range on the northern Albanian border that runs east to west (thus breaking the general geographic trend of the Dinaric system), there is evidence of major glaciation. One geological feature of great importance to the present-day landscape of the Dinarides must be considered in more detail: that of the limestone mountains, often with their attendant faulting. They are hard and slow to erode, and often persist as steep jagged escarpments, through which steep-sided gorges and canyons are cleft by the rivers draining the higher slopes.

Mount Mučanj, lower Dinarides, western Serbia

The most extensive example of limestone mountains in Europe are those of the Karst of the Dinaric Alps. Here, all the characteristic features are encountered again and again as one travels through this wild and underpopulated country. Limestone is a very porous rock, yet very hard and resistant to erosion. Water is the most important corrosive force, dissolving the limestone by chemical action of its natural acidity. As it percolates down through cracks in the limestone it opens up fissures and channels, often of considerable depth, so that whole systems of underground drainage develop. During subsequent millennia these work deeper, leaving in their wake enormous waterless caverns, sinkholes and grottoes and forming underground labyrinths of channels and shafts. The roofs of some of these caverns may eventually fall in, to produce great perpendicular-sided gorges, exposing the water to the surface once more. The gorges of many of the Dinaric rivers, for example those of the Vrbas, Neretva, Tara and Lim, are famous. The partially submerged western Dinaric Alps form the numerous islands and harbours along the Croatian coast.

Only along the Dinaric gorges is communication possible across the Karst, and roads and railways tunnel through precipitous cliffs and traverse narrow ledges above roaring torrents. A number of springs and rivers rise in the Dinaric range, including Jadro Spring noted for having been the source of water for Diocletian's Palace at Split. At the same time, the purity of these rocks is such that the rivers are crystal clear, and there is little soil-making residue. Water quality testing of the Jadro River, for example, indicates the low pollutant levels present. Rock faces are often bare of vegetation and glaring white, but what little soil there is may collect in the hollows and support lush lime-tolerant vegetation, or yield narrow strips of cultivation.

Human activity

Ruins of fortresses dot the mountainous landscape, evidence of centuries of war and the refuge the Dinaric Alps have provided to various armed forces. During the Roman period, the Dinarides provided shelter to the Illyrians resisting Roman conquest of the Balkans, which began with the conquest of the eastern Adriatic coast in the 3rd century BC. Rome conquered the whole of Illyria in 168 BC, but these mountains sheltered Illyrian resistance forces for many years until the area's complete subjugation by 14 AD. More recently, the Ottoman Empire failed to fully subjugate the mountainous areas of Montenegro. In the 20th century, too, the mountains provided favourable terrain for guerrilla warfare, with Yugoslav Partisans organising one of the most successful Allied resistance movements of World War II.

The area remains underpopulated, and forestry and mining remain the chief economic activities in the Dinaric Alps. The people of the Dinaric Alps are on record as being the tallest in the world, with a male average height of 185.6 cm (6 ft 1.1 in) and a female average height of 171.0 cm (5 ft 7.3 in).

Passes

The main mountain passes of the Dinaric Alps are:

• Postojna Gate (Postojnska vrata), Slovenia (606 m or 1,988 ft),
• Vratnik pass, Croatia (850 m or 2,789 ft)
• Debelo brdo, Serbia (1,094 m or 3,589 ft)
• Knin Gate (Kninska vrata), Croatia (about 700 m or 2,297 ft)
• Vaganj, Croatia/Bosnia-Herzegovina (1,137 m or 3,730 ft)
• Ivan-Saddle (Ivan-sedlo), Bosnia-Herzegovina (967 m or 3,173 ft)
• Cemerno, Bosnia-Herzegovina (1,329 m or 4,360 ft)
• Crkvine, Montenegro (1,045 m or 3,428 ft)
• Cakor, Montenegro (1,849 m or 6,066 ft)

Tunnels

Major tunnels transversing the Dinaric Alps include:

• Tuhobić Tunnel, Croatia
• Sveti Rok Tunnel, Croatia
• Mala Kapela Tunnel, Croatia

Mountains and plateaus

Geomorphological subdivisions of Dinaric Alps

The mountains and plateaus within the Dinarides are found in the following regions:

Albania

Maja Jezercë, highest peak Maja Grykat e Hapëta Maja Radohimës Maja e Popljuces Maja Briaset

Maja Hekurave Maja Shnikut Maja Tat Kolata e Mirë

Maja Rosit Maja Kokervhake Maja Shkurt Maja Malësores Maja e Ragamit

Maja Bojs Maja Vukoces Shkëlzen Maja e Kakisë Rrasa e Zogut

Bosnia and Herzegovina

Bjelašnica Cincar Crvanj Čabulja Čvrsnica Dinara, the eponym of the chain. Grmeč Igman

Jahorina Javor Kamešnica Klekovača Konjuh Kozara Lebršnik Lelija

Orjen Osječenica Ozren Maglić (with 2,386 m the highest peak of BiH) Majevica Motajica Prenj Plješivica

Raduša Ravan planina Romanija Trebević Treskavica Šator Trebava Velež

Visočica Vlasulja Vlašić Volujak Vran Vranica Zelengora Zvijezda

Croatia

Dinara Kamešnica Kozjak Mosor Omiška Dinara Biokovo Vrgorsko gorje

Učka Ćićarija Velebit Svilaja Velika Kapela Mala Kapela Žumberak

Kosovo

• Đeravica/Gjeravica
• Gusan/Maja Gusanit
• Marijaš/Marijash

Montenegro

• Bijela gora means "White Mountain" in Montenegrin, which is the opposite of "Crna Gora" or "Black Mountain" which is the local name for Montenegro
• Durmitor
• Orjen
• Zla Kolata (bordering Albania; Kolata e Keq in Albanian)

Serbia

Tara Zlatibor Zlatar Golija Jadovnik Javor Ozren Mučanj

Povlen Radočelo Maljen Čemerno Žilindar Bobija Pešter Giljeva

Jelica Jablanik Medvednik Kamena Gora Jabuka Nemić Čemernica Javorje

Gajeva planina Kukutnica Ovčar Sokolska planina Boranja Pobijenik Murtenica Gradina

Rogozna Subjel Bić Crvena gora Jagodnja Kablar Magleš Kozomor

Jarut Bitovik Golubac Ninaja Banjsko brdo Projić Krstac Drmanovina

Crnokosa Zelena glava Oštrik Crni Vrh Pometenik Malič Blagaja Hum

Zvijezda Drežnička Gradina Mokra Gora Suvobor Gučevo Debela gora Debelo brdo Stojkovačka planina

Slovenia

Gorjanci Kambreško and the Banjšice Plateau The Trnovo Forest Plateau (Slovene: Trnovski gozd), Nanos, and Hrušica Javornik Hills and Snežnik Idrija Hills

Krim Hills and Menišija Bloke The Velika Mountain, Stojna and the Gotenica Mountain The Mala Mountain, the Kočevski Rog and the Poljane Mountain Dry Carniola and Dobrepolje Radulja Hills

Notes and references

Notes:

References:

External links

• Discover Dinarides Project
• Environment for People in the Dinaric Arc Project
• Via Dinarica Trail - Mega-trail across highest peaks of Dinaric Alps