33:
913:
1635:
53:
525:
1621:
1628:
1022:
852:
695:
1168:
60:
583:
With a total length of 96.5 km (60.0 mi) above the ground, and roughly another 90 km (56 mi) below the surface, the Trebšnjica river is one of the longest sinking rivers in the world with the total of 187 km (116 mi) above and under the ground. In hydrological terms, it
1120:, "River of Dubrovnik"). It is only 30 m (98 ft) long but very wide and powerful (average discharge is 24 m/s (850 cu ft/s); on maps it appears as a small bay of the Adriatic, in which it flows, north of Dubrovnik). The lower part of the river is flooded by the sea (
660:
Formation of the Bileća Lake has affected the region significantly, both underground as well as at the ground level, with the extent of ecological impact still, after several decades, not being fully assessed. Entire system of the Trebišnjica wellsprings, its both groups, were part of the
1012:
cave, the largest in Bosnia and
Herzegovina. The river then turns north, curves between the villages of Dvrsnica, Orašje, Čavaš and Turkovići and in the lower Popovo Polje, near the Croatian border, sinks into the several big sinking holes (most notably, the Doljašnica and Ponikva holes.
1152:
The total drainage area of the Trebišnjica covers 4,926 km (1,902 sq mi), of which 600 km (230 sq mi) is shared with the
Neretva drainage area (the spring of Čapljina). The drainage area of the central, longest part of the river covers 2,225 km
1238:
is completed, after an 8 km (5.0 mi) long hydro-energetic tunnel and two reservoirs (with volume of 12,500,000 m (440,000,000 cu ft)) began operating. The power station has a power of 430 MW (two aggregates of 215 MW) and capacity for 619 million kWh
1175:
As a river that flows in geologically unstable terrain (karst) and with such an interrupted flow, the Trebišnjica contains enormous potential for hydroelectricity production. As a result, regulatory works on the Trebišnjica were arguably the most massive ones in the former
812:, flows from the Čemerno mountain also into the Gatačko Polje, next to the villages of Bahori and Gračanica, before it meets the Mušnica near Srđevići. Both streams are characterized by very sharp, almost erratic bends and changes of direction.
611:
zones, geographically and hydrologically distinct albeit in relatively close proximity to each other. In both zones group of wellsprings raises from the underground, consisting of a number of large, abundant founts each.
2333:
2095:
405:
1409:"KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice) - Monitored Effects during and after the Submersion of the Trebišnjica"
642:) at Ćeplica village, is located 3.25 kilometres (2.02 mi) further down the stream from first group. The Čepelica spring-group consists of two main karst hydrological features,
2245:
1128:), 30 m (98 ft) deep and navigable for 3.7 km (2.3 mi) (unlike the upper course of Trebišnjica which is not navigable at all). Several suburbs of Dubrovnik (
1376:"KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice) - 2.3.2. Overview of the Fatničko Polje Karst Outlet Springs"
639:
1242:
1979. To prevent the sinking of the water through the smaller sinking holes in the Popovo Polje, the river bed has been concreted for a length of 67 km (42 mi).
2429:
2424:
1004:
below), right after the
Trebinje. In the field, the river turns northwest, next to the villages of Staro Slano, Đedići, Dobromani, Žakovo, Tulje, Sedlari, Grmljani and
1866:
763:), the Trebišnjica actually represents a very complex system of the above and underground streams. It originates in Bosnia and Herzegovina from two streams from the
1830:
2240:
1876:
1162:
347:
333:
273:
135:
1886:
624:
205:
179:
1931:
1184:
1965. The river was dammed at the village of Gorica, creating artificial lake as an auxiliary water basin for the future hydro-electrical power station (HE)
628:
456:
249:
1906:
1810:
1820:
1795:
620:
108:
1308:"POLJA U KRŠU KROZ KOJA PROTJEČE KASKADNO SU POREDANA OD 950 DO 220 M NAD H | Znate li kako dospijeva do Jadrana najduža bosanskohercegovačka ponornica?"
968:
1765:
817:
666:
635:
1750:
1745:
556:. Before it was utilized for hydro exploitation via various hydrotechnical interventions and systems with different purposes, Trebišnjica used to be a
1805:
1755:
52:
2414:
2266:
1725:
643:
1911:
1825:
1219:; area 33 km (13 sq mi), altitude 400 m (1,300 ft), depth 104 metres (341 ft), volume 1,300,000,000 m (4.6
1408:
1375:
1188:. The water of the lake is conducted by two parallel, 16 km (9.9 mi)-long, hydro-energetic tunnels into the Croatian village of
2007:
1916:
1891:
1790:
2215:
1896:
321:
2404:
1871:
317:
2375:
1482:
2409:
2323:
1104:
After some 20 km (12 mi) of underground flow, the Trebišnjica re-emerges as the powerful spring in the great cave near
665:
landscape, with significant aesthetic value. However entire area surrounding the Trebišnjica river, its headwaters with sources,
2328:
2100:
2318:
678:
677:, formed after construction of the Grnčarevo dam, with the primary purpose of serving as an artificial water reservoir for the
2085:
2080:
2075:
2394:
1605:
785:("Field of Gacko") (from the mountain Lebršnik to Bjelašnica, passes through Lake Klinje and next to the settlements of
2031:
1674:
1578:
1537:
1523:
1347:
899:
742:
881:
724:
2090:
2210:
616:
100:
32:
1483:"KARST HYDROLOGY & HYDROGEOLOGY - The Trebišnjica River Spring-group below Bileća (Vrela Rijeke Trebišnjice)"
873:
716:
1694:
877:
720:
1634:
912:
2184:
1148:) are located alongside the river. Water from the river has been used by the Dubrovnik waterworks since 1437.
442:
1627:
1445:
537:
1231:, two power stations have a power of 422 MW and capacity for production of 2.19 billion kWh yearly.
862:
705:
866:
709:
421:
2399:
1416:
1383:
1815:
549:
81:
1669:
1294:
2419:
1664:
1571:
793:, Srđevići, Bašići, Drugovići, Kula, and Branilovići, before it sinks into the karst in the
1610:
1074:
The waters of the Trebišnjica from the Popovo Polje, re-appear as three separate outflows:
971:, with a small reservoir. The river continues to the west following the southern slopes of
941:
920:
After a total underground flow of some 30 km (19 mi), the waters of the sinking
8:
1141:
588:
2041:
1951:
1490:
928:, which are joined into one river, the Trebišnjica, the most important river in eastern
1946:
797:("Field of Cernica", west of Baba Mountain at the village of Cernica under the name of
2036:
560:, rising and sinking through its course before resurfacing at various places from the
1901:
1533:
1519:
1457:
1343:
1121:
2308:
2065:
1881:
1835:
1564:
1992:
781:
2293:
1850:
1337:
1267:
1145:
1052:
397:
2288:
1987:
674:
615:
The first, at the head of the river and at the outskirts of Bileća town, is the
2158:
2046:
2026:
2002:
1921:
1840:
1740:
1591:
1441:
1257:
937:
1982:
1654:
1307:
945:
2388:
2138:
2128:
1997:
1549:
1461:
1189:
1005:
573:
557:
471:
458:
401:
389:
362:
349:
288:
275:
220:
207:
150:
137:
1620:
1450:
Ekonomska i ekohistorija: časopis za gospodarsku povijest i povijest okoliša
1403:
1401:
1370:
1368:
1366:
983:, Gornja Kočela and Donja Kočela, and enters the largest karst field in the
2355:
2123:
1974:
1333:
1272:
1025:
Ombla catchment area between Bosnia and
Croatia feed of Trebišnjica waters
989:
670:
662:
604:
569:
516:
409:
104:
2298:
2225:
2051:
1775:
1398:
1363:
936:. On the southernmost part of the depression, the river is dammed by the
929:
393:
383:
2261:
1936:
1800:
1760:
1699:
1689:
1684:
1475:
1262:
1129:
1079:
764:
565:
2360:
2280:
2133:
2118:
2017:
1730:
1177:
1009:
972:
955:
The Trebišnjica turns west between the villages of Donje Grnčarevo and
949:
650:
524:
1556:
1446:"Trebišnjica. Jučer najveća ponornica, danas tvornica struje, sutra…?"
768:
2189:
1941:
1098:
1037:
924:
re-appear as a series of very powerful cave springs near the town of
760:
654:
417:
2174:
980:
925:
851:
694:
657:) and springs on the left-bank side of the Čeplica river streambed.
600:
191:
121:
2179:
1926:
976:
577:
1709:
1137:
1108:, in the western part of Dubrovnik. The watercourse is called the
1021:
2143:
1845:
1735:
1587:
1252:
1167:
1133:
1083:
984:
834:
822:
786:
608:
561:
553:
512:
1105:
2194:
1704:
1679:
1659:
1193:
1061:
956:
429:
673:, many villages and productive land is flooded in 1967 by the
2350:
1109:
1094:
790:
756:
545:
413:
1965:
1649:
838:), only to sink again after a short flow above the ground.
1227:
was deconstructed and moved to
Trebinje. Together with HE
932:. The river flows to the south, through the depression of
1436:
1434:
948:. Nearly all of the eastern bank of the lake belongs to
584:
represents a sub-basin within the
Neretva river basin.
1030: Ombla River course and proposed power plant site
779:, flows from the eastern to the western border of the
623:
as primer outflow, and two secondary ones, wellspring
1431:
1156:
1163:
Trebišnjica river damming and regulation controversy
1000:In Popovo Polje, the Trebišnjica used to sink (see
2430:Upper Horizons Hydroelectric Power Stations System
2425:Lower Horizons Hydroelectric Power Stations System
1489:. The Devon Karst Research Society. Archived from
1415:. The Devon Karst Research Society. Archived from
1382:. The Devon Karst Research Society. Archived from
944:and completely flooded upstream by the artificial
2386:
1093:, "boiling water") near the small sea harbor of
603:. The source of the river is a system of strong
1530:Enciklopedijski geografski leksikon Jugoslavije
649:with three main outlets, and group of smaller
619:, consisting of three large wellsprings, with
1572:
599:The Trebišnjica river originate near town of
1332:
1300:
880:. Unsourced material may be challenged and
723:. Unsourced material may be challenged and
420:, b) via group of strong undersea springs (
1579:
1565:
1290:
1288:
1297:, Institute for Statistics of FBiH, p. 34
900:Learn how and when to remove this message
743:Learn how and when to remove this message
2415:Sinking rivers of Bosnia and Herzegovina
2376:List of rivers of Bosnia and Herzegovina
1166:
1020:
911:
523:
1586:
1285:
1089:A series of underwater springs (called
2387:
679:Trebinje-1 Hydroelectric Power Station
2086:Salakovac Hydroelectric Power Station
2081:Grabovica Hydroelectric Power Station
2076:Jablanica Hydroelectric Power Station
1560:
1440:
2101:Čapljina Hydroelectric Power Station
878:adding citations to reliable sources
845:
816:The river shortly re-appears in the
721:adding citations to reliable sources
688:
591:, the river was known as the Arion,
572:coast, and along the coast from the
805:), after a nearby village of Ključ.
59:
13:
2096:Mostar Hydroelectric Power Station
1518:, Third edition (1985); Prosveta;
1339:Through Bosnia and the Herzegovina
1192:, on the Adriatic coast, near the
1157:Damming, regulation and importance
103:is a system consisting of 3 large
14:
2441:
1543:
1342:. Cosimo, Inc. pp. 375–378.
1211:) was constructed, creating huge
552:, and the right tributary of the
388:1) in Bosnia and Herzegovina: to
2405:Rivers of Bosnia and Herzegovina
2091:Rama Hydroelectric Power Station
1633:
1626:
1619:
850:
841:
693:
58:
51:
31:
1016:
684:
16:River in Bosnia and Herzegovina
2410:International rivers of Europe
1326:
1223:10 cu ft)). The old
975:mountain, through the town of
541:
450: • coordinates
341: • coordinates
267: • coordinates
199: • coordinates
129: • coordinates
1:
1516:Mala Prosvetina Enciklopedija
1278:
617:Trebišnjica wellsprings group
607:distributed in two principal
101:Trebišnjica wellsprings group
88:Physical characteristics
1509:
499:The Neretva with Trebišnjica
7:
1550:gornji horizonti (juzni.hr)
1246:
1082:, in the area of the lower
979:and villages of Dražin Do,
916:Trebišnjica in Popovo Polje
491:96.5 km (60.0 mi)
438: • location
425:
329: • location
257: • location
187: • location
117: • location
10:
2446:
2395:Tributaries of the Neretva
1528:Jovan Đ. Marković (1990):
1160:
755:As it flows in an area of
594:
2373:
2343:
2307:
2279:
2254:
2233:
2224:
2203:
2167:
2152:
2109:
2064:
2016:
1973:
1964:
1859:
1783:
1774:
1718:
1642:
1617:
1598:
1295:Statistical Yearbook 2017
1097:in Croatia, northwest of
967:), being dammed again at
508:
503:
495:
487:
448:
436:
382:
378:
363:42.8448369°N 18.3962417°E
339:
327:
312:
308:
304:
289:42.8586959°N 18.4248447°E
265:
255:
244:
240:
236:
197:
185:
174:
170:
166:
151:42.8644525°N 18.4212613°E
127:
115:
96:
92:
87:
77:
72:
46:
42:
30:
21:
472:42.930725°N 17.8321838°E
221:42.862864°N 18.4227204°E
2211:Trebišnjica wellsprings
1153:(859 sq mi).
1078:The powerful spring of
820:, where the village of
528:Trebišnjica in Trebinje
1606:Bosnia and Herzegovina
1532:; Svjetlost-Sarajevo;
1172:
1125:
1086:river, in Hercegovina.
1071:
1036: catchment area,
917:
825:is largest settlement,
640:"Čeplica spring-group"
550:Bosnia and Herzegovina
529:
368:42.8448369; 18.3962417
294:42.8586959; 18.4248447
156:42.8644525; 18.4212613
82:Bosnia and Herzegovina
1487:www.devonkarst.org.uk
1413:www.devonkarst.org.uk
1380:www.devonkarst.org.uk
1203:1967. The dam for HE
1170:
1024:
915:
527:
477:42.930725; 17.8321838
322:Čeplica springs group
226:42.862864; 18.4227204
874:improve this section
808:another stream, the
717:improve this section
408:; and directly into
404:; 2) in Croatia via
111:as primer wellspring
2336:(BiH & Croatia)
1444:(5 November 2012).
605:karstic wellsprings
589:classical antiquity
504:Basin features
468: /
359: /
285: /
217: /
147: /
1173:
1072:
1069: Adriatic Sea
940:at the village of
918:
827:under the name of
530:
2382:
2381:
2369:
2368:
2275:
2274:
2241:Pilažovački Potok
2119:Battle of Neretva
2060:
2059:
1960:
1959:
1887:Bjelimićka Rijeka
1312:www.geovizija.com
1225:Arslanagić bridge
1118:Dubrovačka rijeka
965:Field of Trebinje
942:Gornje Grančarevo
910:
909:
902:
753:
752:
745:
634:The second zone,
522:
521:
418:Dubrovačka Rijeka
37:Trebišnjica River
2437:
2231:
2230:
2165:
2164:
1971:
1970:
1836:Mostarska Bijela
1781:
1780:
1746:Komadinovo Vrelo
1637:
1630:
1623:
1581:
1574:
1567:
1558:
1557:
1503:
1502:
1500:
1498:
1493:on 10 March 2016
1479:
1473:
1472:
1470:
1468:
1438:
1429:
1428:
1426:
1424:
1419:on 10 March 2016
1405:
1396:
1395:
1393:
1391:
1386:on 10 March 2016
1372:
1361:
1360:
1358:
1356:
1330:
1324:
1323:
1321:
1319:
1304:
1298:
1292:
1222:
1070:
1068:
1064:
1059:
1055:
1050:
1046:
1045: limestones
1044:
1040:
1035:
1031:
1029:
961:Trebinjsko polje
905:
898:
894:
891:
885:
854:
846:
775:one stream, the
748:
741:
737:
734:
728:
697:
689:
564:river below the
543:
538:Serbian Cyrillic
483:
482:
480:
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469:
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374:
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62:
61:
55:
35:
19:
18:
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2434:
2385:
2384:
2383:
2378:
2365:
2339:
2310:
2303:
2271:
2250:
2220:
2199:
2157:
2148:
2111:
2105:
2067:
2056:
2012:
1956:
1855:
1821:Konjička Bijela
1796:Živanjski Potok
1770:
1714:
1638:
1632:
1631:
1625:
1624:
1615:
1594:
1585:
1546:
1512:
1507:
1506:
1496:
1494:
1481:
1480:
1476:
1466:
1464:
1452:(in Croatian).
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1420:
1407:
1406:
1399:
1389:
1387:
1374:
1373:
1364:
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1331:
1327:
1317:
1315:
1306:
1305:
1301:
1293:
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1281:
1249:
1220:
1200:is constructed.
1165:
1159:
1066:
1065:
1057:
1056:
1048:
1047:
1042:
1041:
1033:
1032:
1027:
1026:
1019:
922:Fatnička rijeka
906:
895:
889:
886:
871:
855:
844:
829:Fatnička rijeka
749:
738:
732:
729:
714:
698:
687:
661:characteristic
644:Wellspring Čepo
621:Dejanova Pećina
597:
476:
474:
470:
467:
462:
459:
457:
455:
454:
451:
439:
367:
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361:
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155:
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138:
136:
134:
133:
128:
116:
109:Dejanova Pećina
68:
67:
66:
65:
64:
63:
38:
26:
23:
17:
12:
11:
5:
2443:
2433:
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2402:
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2301:
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2258:
2256:
2252:
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2249:
2248:
2243:
2237:
2235:
2228:
2222:
2221:
2219:
2218:
2213:
2207:
2205:
2201:
2200:
2198:
2197:
2192:
2187:
2182:
2177:
2171:
2169:
2162:
2161:of the Neretva
2150:
2149:
2147:
2146:
2141:
2136:
2131:
2126:
2121:
2115:
2113:
2107:
2106:
2104:
2103:
2098:
2093:
2088:
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2078:
2072:
2070:
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2061:
2058:
2057:
2055:
2054:
2049:
2044:
2039:
2034:
2029:
2023:
2021:
2014:
2013:
2011:
2010:
2005:
2000:
1995:
1990:
1985:
1979:
1977:
1968:
1962:
1961:
1958:
1957:
1955:
1954:
1949:
1944:
1939:
1934:
1929:
1924:
1919:
1914:
1909:
1904:
1899:
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1889:
1884:
1879:
1874:
1869:
1863:
1861:
1857:
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1848:
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1838:
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1828:
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647:(Vrelo "Čepo")
638:spring-group (
636:Čepelica river
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859:This section
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842:Middle course
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663:Dinaric karst
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2420:Popovo Polje
2356:Popovo Polje
2344:Other topics
2311:power plants
2267:Tmuški Potok
2153:
2124:Hutovo Blato
2068:power plants
2020:(artificial)
1877:Donji Krupac
1529:
1515:
1495:. Retrieved
1491:the original
1486:
1477:
1465:. Retrieved
1456:(1): 14–28.
1453:
1449:
1421:. Retrieved
1417:the original
1412:
1388:. Retrieved
1384:the original
1379:
1353:. Retrieved
1338:
1334:Arthur Evans
1328:
1316:. Retrieved
1311:
1302:
1273:Hutovo Blato
1235:
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1017:Lower course
1001:
999:
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990:Popovo Polje
988:
964:
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872:Please help
860:
832:
828:
821:
815:
809:
802:
798:
794:
780:
776:
754:
739:
730:
715:Please help
703:
685:Upper course
675:Bilećko Lake
671:Popovo Polje
659:
646:
633:
614:
598:
586:
582:
533:
531:
517:Adriatic Sea
410:Adriatic Sea
107:zones, with
105:karst spring
2400:Trebišnjica
2324:Trebinje II
2226:Tributaries
2204:Wellsprings
2154:Trebišnjica
2042:Salakovačko
1776:Tributaries
1719:Wellsprings
1655:Glavatičevo
1217:Lake Miruša
1213:Lake Bileća
1196:, where HE
1171:Bileća Lake
1008:, near the
946:Lake Bileća
930:Herzegovina
771:mountains:
534:Trebišnjica
509:Progression
475: /
394:Lake Vrutak
366: /
316:wellspring
292: /
248:wellspring
224: /
178:wellspring
154: /
22:Trebišnjica
2389:Categories
2361:Vjetrenica
2319:Trebinje I
2294:Trebinjsko
2281:Reservoirs
2134:Stari Most
2037:Grabovičko
2027:Jablaničko
2018:Reservoirs
1831:Glogošnica
1731:Vrelo Bune
1497:29 October
1442:Lučić, Ivo
1423:21 January
1390:21 January
1279:References
1178:Yugoslavia
1038:limestones
1010:Vjetrenica
1002:Regulation
973:Bjelasnica
950:Montenegro
681:turbines.
651:estavelles
542:Требишњица
496:Basin size
463:17°49′56″E
460:42°55′51″N
406:Cavtat HPP
354:18°23′46″E
351:42°50′41″N
320:, main in
313:4th source
280:18°25′29″E
277:42°51′31″N
245:3rd source
212:18°25′22″E
209:42°51′46″N
175:2nd source
142:18°25′17″E
139:42°51′52″N
25:Требишњица
2334:Dubrovnik
2190:Dubrovnik
2159:sub-basin
2156:drainage:
2047:Mostarsko
2003:Svitavsko
1942:Radobolja
1932:Grabovica
1917:Neretvica
1912:Trešanica
1902:Rakitnica
1892:Slatinica
1826:Idbarčica
1791:Jezernica
1675:Jablanica
1599:Countries
1462:1845-5867
1229:Dubrovnik
1209:Grnčarevo
1198:Dubrovnik
1099:Dubrovnik
1053:dolomites
959:into the
890:June 2018
861:does not
833:River of
810:Gračanica
761:limestone
733:June 2018
704:does not
655:sinkholes
412:: a) via
2329:Čapljina
2262:Čepelica
2216:Čepelica
2180:Trebinje
2112:articles
1998:Deransko
1993:Blatačko
1952:Trebižat
1947:Jasenica
1937:Drežanka
1927:Doljanka
1811:Bukovica
1801:Lađanica
1761:Lađanica
1700:Metković
1690:Čapljina
1685:Počitelj
1670:Ostrožac
1665:Čelebići
1336:(2007).
1263:Trebižat
1247:See also
1236:Čapljina
1205:Trebinje
1186:Trebinje
1142:Prijevor
1130:Mokošica
1122:Croatian
1080:Čapljina
977:Trebinje
765:Lebršnik
578:Sutorina
570:Adriatic
566:Čapljina
73:Location
2289:Bilećko
2144:Zalomka
2110:Related
1988:Boračko
1872:Tatinac
1846:Bregava
1816:Šištica
1736:Bregava
1611:Croatia
1588:Neretva
1510:Sources
1467:28 July
1355:22 June
1318:17 July
1253:Bregava
1239:yearly.
1134:Komolac
1112:River (
1084:Neretva
985:Balkans
882:removed
867:sources
835:Fatnica
823:Fatnica
787:Avtovac
777:Mušnica
769:Čemerno
725:removed
710:sources
609:aquifer
595:Sources
568:to the
562:Neretva
554:Neretva
544:) is a
513:Neretva
428:) near
334:Čeplica
78:Country
2299:Vrutak
2246:Sušica
2195:Cavtat
2175:Bileća
2168:Places
2052:Vrutak
2032:Ramsko
1983:Uloško
1897:Račica
1751:Krupac
1741:Bunica
1705:Opuzen
1695:Gabela
1680:Mostar
1660:Konjic
1643:Places
1590:river
1536:
1522:
1460:
1346:
1194:Cavtat
1146:Lozica
1091:vrulje
1067:
1062:flysch
1060:
1058:
1051:
1049:
1043:
1034:
1028:
1006:Zavala
981:Tvrdoš
969:Gorica
957:Lastva
934:Miruša
926:Bileća
601:Bileća
488:Length
430:Cavtat
426:vrulja
261:Bileća
192:Bileća
122:Bileća
97:Source
2351:Orjen
2255:Right
2185:Ravno
1966:Lakes
1907:Ljuta
1882:Ljuta
1860:Right
1851:Krupa
1710:Ploče
1592:basin
1268:Krupa
1138:Rožat
1126:draga
1116:; or
1114:Umbla
1110:Ombla
1095:Slano
791:Gacko
757:karst
546:river
443:Ravno
416:near
414:Ombla
398:Krupa
384:Mouth
2234:Left
2008:Kuti
1922:Rama
1841:Buna
1784:Left
1650:Ulog
1534:ISBN
1520:ISBN
1499:2018
1469:2020
1458:ISSN
1425:2019
1392:2019
1357:2012
1344:ISBN
1320:2023
1215:(or
1207:(or
1190:Plat
1106:Gruž
865:any
863:cite
767:and
708:any
706:cite
627:and
532:The
392:via
318:Čepo
997:).
876:by
719:by
625:Oko
587:In
580:.
576:to
548:in
180:Oko
2391::
1485:.
1448:.
1433:^
1411:.
1400:^
1378:.
1365:^
1310:.
1287:^
1180:.
1144:,
1140:,
1136:,
1132:,
1124::
987:,
952:.
789:,
669:,
631:.
540::
515:→
424::
1580:e
1573:t
1566:v
1501:.
1471:.
1454:8
1427:.
1394:.
1359:.
1322:.
1221:×
1101:.
993:(
963:(
903:)
897:(
892:)
888:(
884:.
870:.
831:(
801:(
759:(
746:)
740:(
735:)
731:(
727:.
713:.
653:(
536:(
432:.
400:→
396:→
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
