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Dinaric Alps

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632: 652: 955: 157: 525: 42: 675:, 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 666:
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 thinly populated country. Limestone is a very porous rock, yet very hard and resistant to
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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
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that occurred 50 to 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 main tectonic phase of the orogenesis in the area of the Dinaric Karst took place in Cenozoic Era (Paleogene) as a result of the
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This study contributes to an update of average heights among European populations. Our investigation covering 2705 boys and 2842 girls aged 17 years, shows that, contrary to the general belief, adolescents of the Dinaric Alps are, on average, the tallest in Europe. With an average height of
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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 an average male adolescent height of 185.6 cm (6 ft 1.1 in). The people of
425:(Adria) collision with Europe, and the process is still active. The Dinaric Alps were thrown up in more or less parallel ranges, stretching like necklaces from the Julian Alps as far as northern Albania and Kosovo, where the mountainous terrain subsides to make way for the waters of the 539:
limestone and dolomite deposited on top of a huge Bahama-type carbonate platform, while a few kilometers thick carbonate successions have been deformed during the Alpine orogenesis. The main tectonic phase of the Alpine orogenesis in the Dinaric Karst region took place in the
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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
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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
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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.
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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 surface to the water once more.
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Korbar, Tvrtko (2009). "Orogenic evolution of the External Dinarides in the NE Adriatic region: A model constrained by tectonostratigraphy of Upper Cretaceous to Paleogene carbonates".
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Vlahović, Igor; Tišljar, Josip; Velić, Ivo; Matičec, Dubravko (2005). "Evolution of the Adriatic Carbonate Platform: Palaeogeography, main events and depositional dynamics".
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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
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Schmid, Stefan M.; Bernoulli, Daniel; Fügenschuh, Bernhard; Matenco, Liviu; Schefer, Senecio; Schuster, Ralf; Tischler, Matthias; Ustaszewski, Kamil (2008).
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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
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The Dinaric rivers carved many canyons characteristic for Dinaric Alps, and in particular karst. Among the largest and most well known are the
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with their attendant faulting. They are hard and slow to erode, and often persist as steep jagged escarpments, through which steep-sided
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have the highest recorded average of any single country, with 183.9 cm average for men and 171.8 cm for women.
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The Dinaric Alps extend for approximately 645 kilometres (401 mi) along the western Balkan Peninsula from the
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The partially submerged western Dinaric Alps form the numerous islands and harbors along the Croatian coast.
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The Dinaric Alps are one of the most rugged and extensive mountainous areas of Europe, alongside the
367: 2657: 2565:. Montennegro Journal of Sports Sci. Medicine 4 (2015) 1: Original scientific paper. pp. 29–36 943: 17: 2357: 2247: 2213: 605: 499: 474: 2612: 2555: 1624: 1444: 1266: 1940: 1915: 857: 828: 816: 756: 660: 390: 309: 175: 50: 2358:"The Alpine-Carpathian-Dinaridic orogenic system: Correlation and evolution of tectonic units" 1554: 2681: 2221: 2094: 1881: 1954: 1180: 2311: 2273: 386: 2110: 2079: 1518: 1092: 1052: 988: 8: 696: 221: 2315: 2277: 2234: 2088: 2493: 2421: 2380: 2008: 1984: 1801: 1569: 1159: 1096: 930: 924: 812: 601: 573: 374: 347: 233: 1838: 1390: 804: 2532: 2485: 2425: 2302:
Mladen Garasic; Davor Garasic (1 April 2015). "Speleogenesis in Dinaric karst area".
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The mountains and plateaus within the Dinarides are found in the following regions:
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and conglomerates formed by seas and lakes that once covered the area. During the
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are the highest section of the entire Dinaric Alps; this section stretches from
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A1: The area of the North Adriatic - the territory of Istria and the Kras area
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had relatively little direct geologic influence on the Balkans. No permanent
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185.6 cm, they are taller than Dutch adolescents (184 cm on average).
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A8: Coastal and Central Montenegro Mountains - Katunska karst flattening
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conquest of the Balkans, which began with the conquest of the eastern
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A5: The mountains of southern Dalmatia and Mediterranean Herzegovina
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Via Dinarica Trail - Mega-trail across highest peaks of Dinaric Alps
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Vaganj, Croatia/Bosnia-Herzegovina (1,137 m or 3,730 ft)
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Mountain range in the Balkan Peninsula of Southeastern Europe
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Stevo Popović; Gabriela Doina Tanase; Duško Bjelica (2015).
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Pineau, JC; Delamarche, P; Bozinovic, S (1 September 2005).
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A6: The islands of Central and South Adriatic and Peljesac
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and is the most heavily karstified range of the Dinarides.
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coast in the 3rd century BC. Rome conquered the whole of
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Kilibarda, Zoran; Schassburger, Alec (1 October 2018).
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C9: Mountains of the Old Mountains - the central group
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B16: Mountains of High Herzegovina - Mountain range of
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as low as 600 m (1,969 ft). However, in the
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highest peak in Croatia, and second highest of Dinara
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Major tunnels transversing the Dinaric Alps include:
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are cleft by the rivers draining the higher slopes.
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and Southcentral Europe, separating the continental
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Crkvine, Montenegro (1,045 m or 3,428 ft)
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The 455: 2297: 2295: 2585:"Countries with the Tallest Average Heights" 2259: 2257: 535:The Dinaric Karst region is built mostly of 2547: 1367:List of mountains in Bosnia and Herzegovina 1199:C6: Central and Eastern Bosnia Mountains - 1189:C3: Central and Eastern Bosnia Mountains - 366:, standing at 2,694 metres (8,839 ft) 2292: 854:), Slovenia (606 m or 1,988 ft), 646: 2692:Mountain ranges of Bosnia and Herzegovina 2304:EGU General Assembly Conference Abstracts 2254: 1360: 949: 335:of the northeast Italy, downwards to the 1395:highest peak in Bosnia & Herzegovina 978:A9: Mountains of the Montenegrin Rudina 953: 866:, Serbia (1,094 m or 3,589 ft) 650: 630: 523: 144:200,000 km (77,000 sq mi) 2470:Environmental Monitoring and Assessment 1138:B25: The Moravian-Fallen Mountains and 860:, Croatia (700 m or 2,297 ft) 14: 2674: 2263: 815:organising one of the most successful 161:Topography and relief of the Dinarides 1066:B15: High mountains of Herzegovina - 980:A10/11: Mountains of Low Herzegovina 974:A7: Primorje Mountains of Montenegro 511: 498: 468: 449: 346:, where their direction changes. The 2628:, The Columbia Encyclopedia, 6th ed. 2222:participating institution membership 437:The Dinarides are named after Mount 2717:Mountains of Bosnia and Herzegovina 556:, notable for features such as the 136:645 km (401 mi) NW-SE 24: 834: 25: 2738: 2636: 771: 763:, for example, indicates the low 250: 155: 40: 2618: 2605: 2591: 2577: 2504: 2461: 2286:10.1016/j.earscirev.2009.07.004 1792:List of mountains in Montenegro 2439: 2349: 2322: 2240: 2228: 2194: 1111:(Southern Sarajevo Mountains) 671:. Water is the most important 584:. Only the highest summits of 13: 1: 2187: 2070:List of mountains in Slovenia 1785: 1197:C5: Eastern Bosnia Mountains 1195:C4: Central Bosnia Mountains 1020:B7: Massif Lička Plješivica ( 937: 393:. They are formed largely of 2418:10.1016/j.palaeo.2018.06.023 2365:Swiss Journal of Geosciences 2343:10.1016/j.palaeo.2005.01.011 1809:, highest peak in Montenegro 1606:List of mountains in Croatia 1244:List of mountains in Albania 1222:C11: Pre-Dinaric Mountains: 513:[dìnarskòːɡòːrstvòː] 84:2,694 m (8,839 ft) 7: 2712:Mountain ranges of Slovenia 2063: 1872:List of mountains in Serbia 1725:List of mountains in Kosovo 1217:C10: Mountains of Serbia - 639:, lower Dinarides, western 609: 10: 2743: 2697:Mountain ranges of Croatia 2687:Mountain ranges of Albania 2643:Discover Dinarides Project 2529:10.1016/j.crvi.2005.07.004 2067: 1869: 1789: 1722: 1603: 1599: 1364: 1241: 1237: 1219:Podrinje-valjevo mountains 903: 775: 519: 500:[dìnarskòːɡòːrjeː] 429:and the plains of Kosovo. 2707:Mountain ranges of Serbia 2702:Mountain ranges of Kosovo 2482:10.1007/s10661-005-9066-8 2377:10.1007/s00015-008-1247-3 2209:Oxford English Dictionary 1865: 1718: 1212:Zlatarsko-pešterska Group 1070:and Herzegovinian Rudine 843:of the Dinaric Alps are: 596:have glacial valleys and 489: 478: 232: 220: 215: 205: 167: 153: 148: 140: 132: 127: 88: 78: 67: 62: 39: 34: 2648:17 December 2014 at the 2517:Comptes Rendus Biologies 1696: 819:resistance movements of 2727:Physiographic provinces 2722:Mountains of Montenegro 2449:. The Megalithic Portal 2214:Oxford University Press 1207:Polymers-Podrinje Group 946:crosses the mountains. 647:Rivers in Dinaric karst 528:Valbona Pass, northern 451:[alpɛtdinaɾikɛ] 432: 2102: 1886:highest peak in Serbia 1739:highest peak in Kosovo 1361:Bosnia and Herzegovina 1231: 950:Mountains and plateaus 829:Bosnia and Herzegovina 663: 661:Bosnia and Herzegovina 643: 532: 508: 494: 483: 470:[alpidinarike] 465: 456: 446: 418:Alpine earth movements 391:Scandinavian Mountains 310:Bosnia and Herzegovina 176:Bosnia and Herzegovina 51:Bosnia and Herzegovina 2266:Earth-Science Reviews 2095:Trnovo Forest Plateau 2068:Further information: 1870:Further information: 1790:Further information: 1723:Further information: 1604:Further information: 1365:Further information: 1242:Further information: 957: 654: 634: 527: 2248:"Visit Dinaric Alps" 1267:Maja Grykat e Hapëta 1163:B30: Kučke planine ( 1113:B21: Mountain range 944:Belgrade–Bar railway 655:The surroundings of 387:Carpathian Mountains 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1968: 1966: 1963: 1961: 1958: 1956: 1953: 1951: 1948: 1947: 1946: 1942: 1939: 1937: 1934: 1932: 1929: 1927: 1924: 1922: 1919: 1917: 1914: 1912: 1909: 1907: 1904: 1902: 1899: 1897: 1894: 1892: 1889: 1887: 1883: 1880: 1879: 1878: 1877: 1873: 1859: 1855: 1852: 1850: 1847: 1845: 1842: 1840: 1837: 1835: 1832: 1830: 1827: 1825: 1822: 1820: 1817: 1815: 1812: 1810: 1808: 1803: 1800: 1799: 1798: 1797: 1793: 1779: 1775: 1772: 1770: 1767: 1765: 1762: 1760: 1757: 1755: 1752: 1750: 1747: 1745: 1744:Rrasa e Zogut 1742: 1740: 1736: 1733: 1732: 1731: 1730: 1726: 1712: 1708: 1707:Karst Plateau 1705: 1704: 1703: 1702: 1690: 1686: 1683: 1681: 1678: 1676: 1675:Velika Kapela 1673: 1671: 1668: 1666: 1663: 1661: 1658: 1656: 1653: 1651: 1648: 1646: 1643: 1641: 1640:Omiška Dinara 1638: 1636: 1633: 1631: 1628: 1626: 1623: 1621: 1617: 1614: 1613: 1612: 1611: 1607: 1591: 1588: 1586: 1583: 1581: 1578: 1576: 1573: 1571: 1568: 1566: 1563: 1561: 1558: 1556: 1553: 1551: 1548: 1546: 1543: 1541: 1538: 1536: 1533: 1532: 1531: 1527: 1525: 1522: 1520: 1517: 1515: 1512: 1510: 1507: 1505: 1502: 1500: 1497: 1495: 1492: 1490: 1487: 1485: 1482: 1480: 1477: 1475: 1472: 1470: 1467: 1466: 1465: 1461: 1458: 1456: 1453: 1451: 1448: 1446: 1443: 1441: 1438: 1436: 1433: 1431: 1428: 1426: 1423: 1421: 1418: 1416: 1413: 1411: 1408: 1406: 1403: 1401: 1398: 1396: 1392: 1389: 1387: 1386: 1385: 1378: 1375: 1374: 1373: 1372: 1368: 1352: 1351:Maja e Kakisë 1349: 1347: 1344: 1342: 1339: 1337: 1334: 1332: 1329: 1327: 1324: 1322: 1319: 1317: 1314: 1312: 1309: 1308: 1307: 1303: 1302:Kolata e Mirë 1300: 1298: 1295: 1293: 1290: 1288: 1287:Maja Hekurave 1285: 1283: 1280: 1278: 1275: 1273: 1270: 1268: 1265: 1263: 1261: 1255: 1252: 1251: 1250: 1249: 1245: 1235: 1229: 1225: 1220: 1213: 1208: 1202: 1192: 1186: 1182: 1177: 1174:C1: Group of 1172: 1171:Albanian Alps 1166: 1161: 1156: 1151: 1148:B27: Massive 1146: 1141: 1136: 1130: 1125: 1120: 1116: 1110: 1104: 1098: 1094: 1090: 1084: 1079: 1075: 1069: 1064: 1061:B14: Massive 1059: 1054: 1048: 1044: 1039: 1034: 1029: 1023: 1017: 1012: 1006: 1005:Velika Kapela 1000: 994: 990: 985: 982:B1: Group of 956: 947: 945: 932: 929: 926: 923: 920: 917: 914: 911: 910: 909: 898: 895: 892: 889: 886:Kupres Gate ( 885: 882: 879:Ivan-Saddle ( 878: 875: 872: 871:Kninska vrata 868: 865: 862: 859: 856: 853: 849: 848:Postojna Gate 846: 845: 844: 842: 832: 830: 824: 822: 818: 814: 810: 806: 802: 798: 794: 790: 786: 779: 769: 766: 762: 758: 754: 748: 746: 742: 738: 734: 730: 726: 722: 718: 714: 710: 706: 702: 698: 694: 689: 686: 682: 678: 674: 670: 662: 658: 653: 642: 638: 633: 629: 626: 624: 620: 615: 611: 607: 603: 599: 595: 591: 587: 583: 579: 575: 571: 567: 563: 559: 558:Karst Plateau 555: 551: 547: 543: 538: 531: 526: 517: 514: 510: 506: 501: 496: 485: 476: 471: 467: 463: 458: 452: 448: 444: 440: 430: 428: 424: 419: 415: 411: 407: 403: 400: 396: 392: 388: 384: 380: 376: 371: 369: 365: 361: 357: 353: 349: 345: 342: 338: 334: 329: 327: 323: 319: 315: 311: 307: 303: 299: 295: 291: 287: 283: 277: 247: 237: 235: 231: 228: 225: 223: 219: 214: 211: 208: 204: 201: 197: 193: 189: 185: 181: 177: 173: 170: 166: 158: 152: 147: 143: 139: 135: 131: 126: 121: 93: 91: 87: 83: 81: 77: 73: 70: 66: 61: 56: 52: 48: 43: 38: 33: 30: 19: 2682:Dinaric Alps 2626:Dinaric Alps 2625: 2620: 2613:Dinaric Alps 2611:Summitpost. 2607: 2593: 2579: 2567:. Retrieved 2562: 2549: 2540: 2523:(9): 841–6. 2520: 2516: 2506: 2473: 2469: 2463: 2451:. Retrieved 2441: 2429:. Retrieved 2409: 2403: 2393: 2368: 2364: 2351: 2334: 2330: 2324: 2307: 2303: 2269: 2265: 2242: 2230: 2207: 2196: 2167:Dry Carniola 2158:Kočevski Rog 2014:Banjsko brdo 1885: 1805: 1738: 1619: 1394: 1381: 1380: 1341:Maja Vukoces 1292:Maja Shnikut 1282:Maja Briaset 1260:highest peak 1259: 1257: 1254:Maja Jezercë 1233: 1176:Kočevski Rog 1026:B8: Massive 1009:B5: Massive 993:Gorski kotar 984:Trnova herod 941: 907: 887: 880: 870: 858:Vratnik pass 851: 838: 825: 821:World War II 781: 778:Dinaric race 753:Jadro Spring 749: 737:Cem/Ciijevna 690: 665: 627: 542:Cenozoic Era 534: 436: 372: 364:Maja Jezercë 358:and eastern 330: 298:Adriatic Sea 281: 246:Dinaric Alps 245: 243: 234:Type of rock 227:Mesozoic era 72:Maja Jezercë 35:Dinaric Alps 29: 2569:4 September 2431:23 November 2412:: 112–127. 2371:: 139–183. 2054:Debelo Brdo 2049:Debela gora 1941:Kamena Gora 1854:Sinjajevina 1814:Bijela gora 1680:Mala Kapela 1321:Maja Shkurt 1135:Sinjajevina 1016:Mala Kapela 942:The famous 869:Knin Gate ( 864:Debelo brdo 761:Jadro River 333:Julian Alps 238:Sedimentary 222:Age of rock 210:Julian Alps 115: / 90:Coordinates 2676:Categories 2224:required.) 2188:References 2171:Dobrepolje 2125:Krim Hills 1882:Mokra Gora 1807:Zla Kolata 1786:Montenegro 1764:Guri i Kuq 1540:Treskavica 1514:Plješivica 1484:Osječenica 1400:Bjelašnica 1311:Maja Rosit 1109:Bjelašnica 1022:Plješevica 938:Rail lines 881:Ivan-sedlo 805:Montenegro 787:resisting 776:See also: 743:, and the 610:Prokletije 582:glaciation 427:Drin River 360:Montenegro 318:Montenegro 206:Borders on 188:Montenegro 128:Dimensions 74:in Albania 55:Montenegro 2453:19 August 2426:134665429 2310:: 10058. 2203:"Dinaric" 2085:Kambreško 1980:Murtenica 1975:Pobijenik 1955:Čemernica 1936:Medvednik 1735:Gjeravica 1625:Kamešnica 1585:Zelengora 1450:Klekovača 1445:Kamešnica 1336:Maja Bojs 1226:(NW) och 1150:Bjelasica 1145:Ljubišnja 1083:Zelengora 1043:Klekovača 995:plateaus 960:Legend: 933:, Croatia 927:, Croatia 921:, Croatia 915:, Croatia 839:The main 785:Illyrians 765:pollutant 729:Komarnica 697:Rakitnica 681:sinkholes 566:limestone 546:Paleogene 414:sandstone 410:limestone 296:from the 282:Dinarides 168:Countries 149:Geography 112:45°N 17°E 80:Elevation 2658:Archived 2646:Archived 2563:mjssm.me 2537:16168365 2498:21572417 2490:17054013 2385:55108896 2160:and the 2146:and the 2129:Menišija 2087:and the 2080:Gorjanci 2064:Slovenia 2034:Zvijezda 2024:Crni Vrh 1911:Jadovnik 1896:Zlatibor 1884:– 1819:Durmitor 1804:– 1759:Majrashi 1737:– 1685:Žumberak 1660:Ćićarija 1618:– 1590:Zvijezda 1560:Vlasulja 1555:Visočica 1535:Trebević 1524:Romanija 1499:Motajica 1494:Majevica 1469:Lebršnik 1435:Jahorina 1420:Čvrsnica 1393:– 1382:range's 1379:– 1346:Shkëlzen 1297:Maja Tat 1228:Majevica 1201:Jahorina 1185:Gorjanci 1181:Žumberak 1129:Durmitor 1078:Lebršnik 1058:Čvrsnica 1045:(S) and 1001:plateau 793:Adriatic 709:Sutjeska 685:grottoes 598:moraines 586:Durmitor 578:ice caps 550:Mesozoic 537:Mesozoic 484:Dinaridi 479:Динариди 443:Albanian 406:dolomite 399:Cenozoic 395:Mesozoic 383:Pyrenees 302:Slovenia 290:Southern 284:, are a 280:), also 200:Slovenia 18:Dinaride 2312:Bibcode 2274:Bibcode 2235:Profile 2120:Snežnik 2111:Hrušica 2099:Slovene 2039:Suvobor 2009:Golubac 1985:Gradina 1960:Javorje 1834:Maganik 1670:Svilaja 1665:Velebit 1645:Biokovo 1600:Croatia 1580:Vranica 1570:Volujak 1504:Manjača 1415:Čabulja 1238:Albania 1160:Visitor 1140:Maganik 1103:Vranica 1097:Volujak 1011:Velebit 989:Snežnik 904:Tunnels 811:, with 797:Illyria 693:Neretva 677:caverns 669:erosion 623:canyons 554:Balkans 530:Albania 520:Geology 505:Slovene 462:Italian 457:Dinaret 352:Albania 326:Albania 306:Croatia 216:Geology 180:Croatia 172:Albania 2559:(.pdf) 2535:  2496:  2488:  2424:  2383:  2156:, the 2144:Stojna 2109:, and 2044:Gučevo 2019:Krstac 2000:Magleš 1995:Kablar 1990:Subjel 1950:Jabuka 1931:Pešter 1926:Bobija 1906:Golija 1901:Zlatar 1866:Serbia 1849:Rumija 1839:Njegoš 1829:Lovćen 1749:Gusani 1719:Kosovo 1630:Kozjak 1616:Dinara 1565:Vlašić 1519:Raduša 1474:Lelija 1460:Kozara 1455:Konjuh 1410:Crvanj 1405:Cincar 1391:Maglić 1384:eponym 1377:Dinara 1230:(SE). 1224:Kozara 1203:Group 1193:Group 1191:Vlašić 1187:Group 1165:Žijovo 1155:Komovi 1119:Vojnik 1115:Golija 1105:Group 1099:Group 1093:Maglic 1085:Group 1074:Crvanj 1053:Raduša 1038:Cincar 1028:Dinara 999:Notran 817:Allied 739:, the 735:, the 733:Morača 731:, the 727:, the 723:, the 719:, the 715:, the 711:, the 707:, the 703:, the 699:, the 695:, the 641:Serbia 637:Mučanj 635:Mount 619:gorges 570:Dinara 439:Dinara 356:Kosovo 344:massif 322:Kosovo 320:, and 314:Serbia 196:Serbia 192:Kosovo 133:Length 117:45; 17 2494:S2CID 2422:S2CID 2381:S2CID 2361:(PDF) 2218: 2134:Bloke 2107:Nanos 1965:Ovčar 1921:Ozren 1916:Javor 1844:Orjen 1824:Hajla 1697:Italy 1635:Mosor 1550:Velež 1545:Šator 1509:Prenj 1489:Ozren 1479:Orjen 1440:Javor 1430:Igman 1425:Grmeč 1169:B31: 1158:B29: 1153:B28: 1143:B26: 1133:B24: 1131:area 1127:B23: 1122:B22: 1107:B20: 1101:B19: 1087:B18: 1081:B17: 1068:Velež 1063:Prenj 1056:B13: 1051:B12: 1047:Grmeč 1041:B11: 1036:B10: 1033:Šator 789:Roman 713:Vrbas 705:Drina 701:Prača 594:Prenj 590:Orjen 562:karst 341:Korab 184:Italy 47:Orjen 2571:2016 2533:PMID 2486:PMID 2455:2012 2433:2022 2169:and 2152:The 2138:The 2127:and 2118:and 2093:The 1891:Tara 1655:Učka 1575:Vran 1179:C2: 1089:Bioč 1049:(N) 1031:B9: 997:B3: 991:and 987:B2: 745:Drin 725:Tara 721:Piva 717:Ugar 683:and 657:Foča 621:and 592:and 433:Name 397:and 389:and 379:Alps 339:and 244:The 198:and 141:Area 103:17°E 100:45°N 68:Peak 53:and 2525:doi 2521:328 2478:doi 2474:123 2414:doi 2410:506 2373:doi 2369:101 2339:doi 2335:220 2282:doi 2105:), 2029:Hum 741:Lim 487:or 454:or 404:of 354:to 337:Šar 324:to 288:in 2678:: 2561:. 2539:. 2531:. 2519:. 2515:. 2492:. 2484:. 2472:. 2420:. 2408:. 2402:. 2379:. 2367:. 2363:. 2333:. 2308:17 2306:. 2294:^ 2280:. 2270:96 2268:. 2256:^ 2206:. 2142:, 2101:: 1256:- 1183:/ 1167:) 1024:) 823:. 747:. 679:, 659:. 608:: 588:, 564:– 516:. 507:: 503:; 481:, 477:: 473:; 464:: 460:; 445:: 412:, 408:, 385:, 381:, 377:, 362:. 316:, 312:, 308:, 304:, 267:ær 194:, 190:, 186:, 182:, 178:, 174:, 2601:. 2587:. 2573:. 2527:: 2500:. 2480:: 2457:. 2435:. 2416:: 2387:. 2375:: 2345:. 2341:: 2318:. 2314:: 2288:. 2284:: 2276:: 2250:. 2216:. 2097:( 1262:) 1258:( 1117:- 1095:- 1091:- 1076:- 1007:) 850:( 604:( 544:( 276:/ 273:k 270:ɪ 264:n 261:ˈ 258:ɪ 255:d 252:/ 248:( 20:)

Index

Dinaride

Orjen
Bosnia and Herzegovina
Montenegro
Maja Jezercë
Elevation
Coordinates
45°N 17°E / 45°N 17°E / 45; 17

Albania
Bosnia and Herzegovina
Croatia
Italy
Montenegro
Kosovo
Serbia
Slovenia
Julian Alps
Age of rock
Mesozoic era
Type of rock
/dɪˈnærɪk/
mountain range
Southern
Balkan Peninsula
Adriatic Sea
Slovenia
Croatia
Bosnia and Herzegovina

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