Coordinates: 42°34′08″N 18°32′56″E / 42.56889°N 18.54889°E / 42.56889; 18.54889
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View of Orjen with peaks Veliki kabao (right) and Vučji zub (left)
Highest point
Elevation1,895 m (6,217 ft)
Coordinates42°34′08″N 18°32′56″E / 42.56889°N 18.54889°E / 42.56889; 18.54889
Parent rangeDinaric Alps
Age of rockCretaceous
Mountain typeFold mountain
Type of rockGlaciokarst
Mt. Orjen topographic map
Broader region of Orjen and Bay of Kotor. 7 August 2001.
Orjen is located in the South-east Dinaric Alps
Cirque Borovi do in the north at Bijela gora

Orjen (Serbian Cyrillic: Орјен, pronounced [ɔ̂rjɛn]) is a transboundary Dinaric Mediterranean limestone mountain range, located between southernmost Bosnia and Herzegovina and southwestern Montenegro.

Its highest peak is Veliki kabao, which stands at 1,895 m (6,217 ft). The Orjen Peak is the highest peak in the Sub-Adriatic Dinarides. The massif of Orjen lies east to south-east of Trebinje in Bosnia and Herzegovina and north-west of Risan in Bay of Kotor (Boka Kotorska). From the town of Risan, situated at the innermost protected part of the bay, a well-engineered road, at first metalled, with many hairpin bends climbs to about 1600 m, over to the interior. At the main summit of Orjen and the surrounding ridges and high plateaus the action of quaternary glaciation is evident. During the Ice Age, long valley glaciers receded from Orjen to the Bay of Kotor and surrounding poljes. Hollowing U-shaped valleys and cirques in their course. Glaciers also shaped jagged peaks and ridges. Glacial and karst type relief combine now in a unique coastal scenery. There are few places elsewhere in the Mediterranean which demonstrate similar phenomena.

The Natural and Culturo-Historical Region of Kotor is a UNESCO World Heritage site, comprising the territory between Orjen and Lovćen, including all the small towns in the bays of Risan and Kotor with their natural setting. With this privileged natural harbour the Bay of Kotor has been settled for millennia. Illyrians[citation needed] and Greeks[citation needed] colonised the coast from 400 BC and established today's ports Risan (Rhizon) and Kotor (Cattaro). Due to lack of potable water, the high mountain was never densely populated. Snow patches collected from deep pit holes were used even late in the 20th century to provide the few hamlets with water. Today, wells are used instead.


Mount Orjen is a block mountain lifted up as a horst and thus towering above the lowered Bay of Kotor and the high karst plateaux surrounding the Mount Orjen horst. With 1895 m difference between the lowest and the highest point, relief energy has a great role in the extremely harsh environment. A hyperkarstic barren landscape of vast karren fields contrasts with very species rich vegetation types, ranging from evergreen deciduous forests at lower altitudes to endemic calcareous Dinaric Fir and Pine forests in higher altitudes. Precipitation reaches 5000 L per m2, amounts typical for tropical rainforests or the eastern Himalayas than the dry Mediterranean. Lying at Europe's wettest coast, snow easily accumulates on karstic plateaux and as late as June small snow patches continue to lie in shaded places under the summits. Skiing is possible but no relevant infrastructures exist today. Orjen is a more important hiking destination. Three mountain huts provide basic accommodation.

Orjen comprises transboundary area of about 400 km2 between Bosnia and Herzegovina and Montenegro, and runs for 25 km from region around Trebinje in Bosnia and Herzegovina in the north-west, to Bay of Kotor in Montenegro in the south-east. Mount Orjen is composed of four high karstic plateaux divided by ridges. Three near parallel ridges collide in Veliki kabao, Orjens' culmination point. The ridges are arranged by elevation with the highest to the north screening the Bijela gora plateaux from the Mediterranean coast. The separated plateaux are the Krivošije to the East, Bijela gora to the North, and Dobri do and Vrbanj to the West. Only few settlements are scattered in surrounding poljes. The poljes of Grahovo, Dragalj, Vrbanj, Krusevica and Grabalj are important for agricultural use and provide the only lines of communication in the karst. Migration circled around Mount Orjen as a major obstacle between the coastal, Herceg Novi and Risan and the interior towns of Grahovo, Trebinje and Nikšić.

Several dry river valleys are found on Orjen. Only in decades they react as short-living rivers when heavy rain and snow-melt combine. Flooding can be a problem and several poljes are renowned for their long inundation periods.

Glacial traces[edit]

Mediterranean mountains bear no glaciers any more except small snow fields in some shaded cirques of the Taurus range. Even during the pleistocene snowlines were not much lower as in today's Alps. Glaciers were only of local significance in the Mediterranean enabling frost sensitive vegetation types to survive the climate changes of the Quaternary. Among the once glaciated Mediterranean mountains Orjen was outstanding for one of the biggest ice cap in the region. A 150 km2 covered 1/3 of the area. All part above 900 m were buried under a thick sheet of ice from where several glacial tongues descended to 500 m above sea level. Traces of glacial activity are evident in any part of Orjen as in the Bijela gora plateaux. No glacial lakes survive today as they were extinguished due to the porosity of the karstified landscape. Many cirques, U-shaped valleys and moraines and jagged ridges and summits bear the evidence of the glacial erosion. In stoneage and Bronze Age humans settled in the Orjen region. This early human activity is depicted by rock paintings of deerhunt and humans in Lipci in Risan bay. A major Bronze Age excavation site is at Popovo polje to the north of Mount Orjen.

Snow lines across the Mediterranean. The upper line shows recent snowlines the bigger signifies those from the last Ice age. Mount Orjen due to heavy precipitation was in Ice age a major center of the Mediterranean local glacier formation


Karst fauna on Orjen

Mount Orjen is built up from pure Cretaceous limestone. As precipitation and temperatures are high and vegetation is abundant karstification processes are evolved. Lapies, sinkholes and caves resolve from the solution of the limestone. The solution process is the faster the more water is available for solution. Vegetation and soilformation play also a role in the process. A major disadvantage is that the water is percolating fast in the porous rocks and does not form brooks and rivers despite the heavy amounts of precipitation. An overall dryness is characteristic that is unsuitable for settling. Thus the region has been depopulated for a long time. Only during times of repression the unfavourable high mountains were mainly populated by Montenegrin tribes. During the time of the Ottoman rule from the 15th to the 19th century the high karst was acting as main shelter for the Christian population. Military campaigns of Ottomans and Austro-Hungarians faced heavy losses while both great powers underestimated the difficulties to undertake successful raids in karst areas. The Battle of Vučji Do between Montenegrins and Turks and the Krivošije uprising in 1869 showed that the Montenegrins used the natural conditions in their favour.

Karst is also a major tourist attraction as caves are frequent and peculiar geomorphological forms can be studied. Karst vegetation on the other hand is species rich and major karst areas are hot spots of biodiversity. The both famous Southeast Asian karst areas like the Guilin tower karst region in Southern China or Phuket island in Thailand and the Mediterranean dinaric karst areas with the Plitvice lakes in Croatia and the Bay of Kotor in Montenegro rival with spectacularity.


Tectonically the area of the Southern Adriatic is very active as the frequency of earthquakes indicates. As the Adriatic Plate subduces under the Dinarids, earthquakes can have devastating energy. Sometimes even tsunamis are observed. Mount Orjen is completely built of folded Cretaceous limestones which belongs to the High-Karst Zone geological unit. The High-Karst Zone has the greatest extent in the territory of Montenegro. The terrain of this geotectonic unit is mainly built up of Mesozoic (Triassic, Jurassic and Cretaceous) limestones and dolomites of several kilometres of thickness. This thickness is even larger, due to the reverse faulting and overthrusting and thus repeating of carbonate series. The karst of this region is characterised by all surface occurrences and all processes characteristic for holokarst such as: karst plain, polje, uvala, sinkhole, dry-, hanging-, blind- and karstified valley, lapies, canyon, shaft, cave, resurgence, vrulja, estavelle and so on. The karstification of limestones and dolomites in this area is below the base level of erosion, below the sea level and is deeper than 1,000 m. The High-Karst Zone has all the prominent characteristics of fluvial erosion (deep canyons of Komarnica and Morača rivers with their tributaries), glacial erosion (on Mount Orjen), lacustrine, sea and combined erosion.

Along the internal belt of Bay of Kotor, from Morinj, across Risan to Kotor, the High-Karst Zone is in direct contact with the sea, as the High-Karst Zone overthrusts the Pindus Cukali Zone where Mount Orjen rises from the Bay of Risan. The direct contact of the Adriatic sea and the High-Karst Zone leads to interesting hydrological phenomena. In these terrains the largest vrulja on the Adriatic coast, called Sopot, is located. The vast differences in water-yielding capacity of the constant and periodic karst springs point out to the strong karstification of High-Karst Zone limestones and dolomites on Mount Orjen. The difference between minimal and maximal water yielding capacity is over 350 m³.


Orjen is within the Mediterranean subtropical belt. While summers are hot and sunny, autumn, winter and spring are rainy seasons. It is the climate type of the Mediterranean but modifications exist in the vast region. For exymple sinkholes may create local areas with continental microclimates as is the cas with the Borovi do and Opuvani do, where frequent freeze-thaw cycles create favourable conditions for arcto-alpine and alpine biota. A peculiarity of the littoral Dinarids is the precipitation regime as Orjen receives Europe's' most heavy precipitation. Like the monsoon rain is seasonally distributed, thus November thunderstorms sometimes pour 2000 L of water in several days, while August is frequently completely dry leading to forest fires. With a maximum discharge of 200 m³/s water one of the biggest karst springs, the Sopot spring, is a remarkable indicator of this seasonality. Most of the time it is inactive but after heavy rain a remarkable waterfall appears 20 m above the Bay of Kotor.

Station Height [m] Type Character Precipitation [mm] Snow
Veliki kabao 1895 Dfsc perhumid Mediterranean snowclimate about 6250 ap. 140 days
Crkvice 940 Cfsb (fs= without summerdryness), perhumid Mediterranean mountain climate 4926 70 days
Risan 0 Csa (s= double winter rain season), perhumid Mediterranean coast climate 3500 2 days

* classification scheme after Köppen

Two wind systems are noteworthy for their ecological significance: Bora and Sirocco. Strong cold downslope winds of Bora type appear in winter and are most severe in the Bay of Risan. Gusts reach 250 km/h and can lead to a significant fall of temperatures in several hours with freezing events problematic for most of the Mediterranean cultures. Bora weather situations are frequent and sailors keep an eye on the mountains as cap clouds indicate an imminent Bora event. Sirocco is a warm humid rain and is important as it brings heavy rain. It appears throughout the year but is usually centered in autumn and spring.

Station Period Height [m] I II III IV V VI VII VIII IX X XI XII I-XII [mm/m2a]
Herceg Novi 1961–1984 40 230 221 183 135 130 73 28 45 160 181 326 262 1974
Risan 1961–1984 40 405 342 340 235 153 101 66 123 188 295 423 434 3105
Grahovo 1961–1984 710 351 324 305 251 142 94 55 103 202 416 508 473 3224
Podvrsnik 1961–1984 630 407 398 367 305 151 101 77 132 238 465 593 586 3820
Vrbanj 1961–1984 1010 472 390 388 321 181 104 70 122 224 369 565 536 3742
Knežlaz 1961–1984 620 547 472 473 373 207 120 72 136 268 400 629 661 4358
Crkvice 1961–1984 940 610 499 503 398 198 135 82 155 295 502 714 683 4774
Ivanova Korita 1960–1984 1350 434 460 742 472 128 198 74 46 94 300 694 972 4614
Goli vrh 1893–1913 1311 271 286 307 226 188 148 75 70 215 473 415 327 3129
Jankov vrh 1890–1909 1017 424 386 389 346 212 124 55 58 202 484 579 501 3750
Cetinje 1961–1984 655 434 357 367 288 164 92 72 118 209 306 489 498 3394
Grab-Zupci 1934–1960 677 333 325 257 195 183 83 59 86 173 360 447 485 2985
Trebinje 1931–1960 276 193 190 160 102 119 70 43 76 110 239 247 249 1762
Dubrovnik 1931–1960 49 147 113 102 92 79 60 24 38 97 156 213 186 1307

* monthly and yearly precipitation ranges in Dalmatia, Herzegovina and Montenegro



Mostly limestone rocks but also moraines and screes. Coastal cliffs are present at all parts of the Bay of Kotor. Many forest types can be seen of which Mediterranean deciduous evergreen don't play a significant role. Dinaric calcareous fir forests are found in several grooves on the Bijela gora but are difficult to reach. Bosnian pine forests are quite widespread on all major ridges. Virgin woodlands still exist, mainly Beech forests.


Zone [m] Type Vegetation (Biotopes)
0- 400 Mesomediterranean ME= Meridional (subtropic belt) Rusco-carpinetum (Ruscus aculeatus, Carpinus orientalis), Orno-Quercetum ilicis (Quercus pubescens, Quercus cerris, Juniperus communis, Quercus ilicis), Nerion oleandri (Nerium oleander)
400- 1,100 Supramediterranean SME= Suprameridinal (subtropic belt) Quercus trojana (Quercus trojana), Carpinus orientalis (Carpinus orientalis), Petterio-Quercetum confertae (Fuk.) Lov. (Petteria, Quercus conferta), Castaneo-Quercetum pubescentis (Anic) Lov. (Castanea sativa, Quercus pubescens), Seslerio-Ostryetum carpinifoliae Horv. (Sesleria sphaerocephala, Sesleria caerulea, Ostrya carpinifolia)
1,100- 1,450 Oromediterranean NE= Nemoral (temperate zone) Seslerio autumnalis–Fagetum (Horv.) Wrab. (Sesleria autumnalis, Fagus sylvatica), Pinion heldreichii (Pinus heldreichii), Oreoherzogio-Abietetum illyricae Fuk. (basic soil, Abies alba), Seslerio autumnalis–Abietetum illyriacae (Horv.) Fuk.
1,450- 1,700 Altimediterranean BO= Boreal (taiga zone) Fago-Pinetum heldrecihii Jank. (Fagus sylvatica, Pinus heldreichii), Seslerio robustae-Juniperetum hemisphaericae (Hor.) Kus. (Sesleria robusta, Juniperus communis ssp. Haemispherica), Lonicero-Rhamnion Fuk. (Lonicera nigra, Lonicera alpigena, Rhamnus), Amphoricarpion neumayerii (Horv.) Lak. (Amphoricarpos neumayerii)
1,700- 1,900 Cryomediterranean AL= Alpine (tundra zone) Trifolio Polganetalia Quéz (Trifolium), Narcisso-Gentianetum nivalis Lov. & Rac (Narcissus, Gentiana nivalis), Drabo-Androsacetalia Quéz (Draba hoppeanae, Androsace alpina), Muscaro-Scillion nivalis Quéz
Vegetation profile on Orjen

Across Orjen vegetation varies with climate and altitude. While the sub-adriatic range exhibits evergreen deciduous forests, the vegetation graduates to temperate forests, conifers and tundra in the northern and upper regions. The ridges also have a variety of Mediterranean alpine vegetation – oromediterranean pastures. The typical karst country with bare limestone rochocks interspersed with parches of wood is found on lower altitudes. White Oak, Hop-hornbeam and Montpellier Maple, or the characteristic scrub of the maquis shrubland and garrigue are notable. There are stony meadows in the sunken dolina of the karst that contrast vividly with the stony slopes and rocky scrubland all round. Higher altitudes are characterised by heavy beech forest with occasional open grassy pastures. On northern branches silver fir accompanies beech. Above the beech and fir-beech forests are scattered open stands of pure Dinaric calcareous Silver Fir forests and Bosnian pine with deep-purple young cones set among stiff light-green needles. Open stony screes and rocks are exposed to the jagged ridges and summits. They are very rich in species.


Flora is of Balkan type with many Illyrian and Balkan endemics. Notable is local endemism with 10 endemics restricted to Mount Orjen.



A National Park was planned for a long time on Orjen. The disintegration of Yugoslavia, civil war and standstill of tourism cancelled plans. Today plans a rejuvenated but funding maybe a problem. UNESCO declared the Natural and Culturo-Historical Region of Kotor a World Heritage site. The part of Orjen within the boundaries of this Site is namely the Krivosije plateaux. A further evaluation of the patrimony and nomination of a greater part of Orjen as National park has good reasons. Unique flora, fauna and relief certainly require a protection plan by administrative action.


The earliest historic confirmations are the Lipce rock paintings which are dated in the Bronze Age. The first historic significant events are connected with the Illyrians when Queen Teuta, reigned approximately from 231 BC to 228 BC choose Risan as her capital during her war against the Romans. The Greek also colonised the region and eventually the Romans took over. The classical name of the Bay of Kotor is after Rhizon (Risan) Sinus Rhizonicus. Eventually Kotor was becoming more important during the Middle Ages


Shepherds on Orjen. Dried mushrooms decorate the walls in this hut

Only few traditional shepherds live today on Orjen. Mostly remain on the northern side of the Bijela gora. They have their local songs describing life on the remote mountain and every year in July a great feast takes place when all the shepherds from Bijela gora come together to sing dance and eat on a pasture at Ledenik.

Livestock is mostly sheep but also horses and few cattle are held. At Orjen saddle oxen graze. In former times nomadic migration took place between the poljes and the higher regions of Orjen. The traditional housing on Orjen is the so-called Koliba. Small limestone huts with roofs build of pine bark. Only few hamlets are inhabited, mostly close to the coast. The higher up the stronger the push factors acted to leave. Tribes on Orjen were once renowned for their wildness and still people from the coast have this notion towards the mountain tribes.


Glacial and karst features compose a unique landscape that is attracting visitors also from abroad. Backpacking and alpine recreation are important factors for the development of the Orjen region. Three mountain huts are established and enthusiasts keep winter sports alive.


Ascend on Orjen via the Medugorje valley

Trails are maintained by the PSD Subra mountaineering association from Herceg Novi. Most trails are around the huts at Vratlo (1160 m) and Orjen ridge (1594 m). 40 km of marked trails exist in the Mount Orjen region, leading to the most attractive destinations. Marked trails start at the city bus station at Herceg Novi (30 m) and lead to the Vratlo hut (1160 m). Hiking in other more remote parts is also possible but no marcation currently exists. Visitors of Bijela gora or Dobri can use several local forest roads. sometimes shepherds can offer night accommodation.

Water is only available at some places, shepherd villagers usually use rain collectors. Most hikers tend to visit Subra (1680 m) or Veliki kabao (1895 m). Both are well marked.

Brown bears appear in the Bijela gora and should not be disturbed as the population is critically endangered.

Every year around mid May a half marathon called Orjen marathon is organised by the PSD Subra alpine organization. Guests are welcomed to take part in the traditional manifestation


Several interesting alpine like climbing possibilities like rock climbing exist. Most remarkable is the 500 m wall of the Subra amphitheatre. In last few years the alpine – speleo section (A.S.O.S.) of PSD Subra started to climb routes on Mount Orjen. Good climbing routes are only 10 minutes walk from the Vratlo mountain hut. Other good climbing routes are in Subra's Amphitheatre and Reovacka Greda rocks. Mount Orjen gives a lot opportunities for climbing unclimbed routes with various difficulties.

Major Peaks
Peak Height (m) Character Difficulty
Veliki kabao 1,894 rock scramble, wall, scree difficult north approach, alpine character, scree on east
Velika Jastrebica 1,865 trail easy trail
Buganja greda 1,849 rock scramble, scree basic rock scramble, difficult slippery scree on north side
Visoki brijeg 1,833 rock scramble, scree, trail basic rock scramble, scree on north
Vučji zub 1,805 rock scramble scree, wall scree on east, difficult rock crevices on north
Borovik 1,777 rock scramble, scree difficult scree on north,
Međugorje 1,769 rock scramble, wall difficult major wall from north, south and west
Goliševac 1,721 rock scramble, scree difficult scrre from north
Markov kuk 1,721 rockscramble, trail, scree basi scramble
Pazua 1,680 rock scramble, wall difficult rock scramble
Subra 1,679 rock scramble, big wall 500 m wall still unclimbed

Summer activities[edit]

  • Backpacking – Between late spring and early fall. All overnight trips into the back country require sufficient water supplies due to limited water sources available.
  • Bicycling – Mountain biking is possible throughout Mount Orjen and local roads are well suited for cycling.
  • Swimming – Orjen is located near the Bay of Kotor on the Adriatic coast.
  • Orjen marathon – Annual sport event with several possible tracks, starting from the Vratlo mountain hut towards Subra (1679m) and Veliki kabao (1895m) peaks.

Winter activities[edit]

Much of Mount Orjen is inaccessible due to heavy snow in winter. However, Orjen saddle 1594 m can be reached in winter from Vrbanj.

  • Skiing – the only skiing area is around Orjen saddle opens in winter. No lifts and equipment are provided at the mountain hut.
  • Hunting – Hunters are generally welcome official permits are required.


  • Pavle Cikovac: "Sociology and ecology of Silver Fir forest on Mt. Orjen – Montenegro". LMU Munich (2002), Department of Geography