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Southern Carpathians

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Units. The Getic Nappe was identified by Murgoci (1905), while the general understanding over the Alpine structure of the South Carpathians was later refined by Codarcea (1940), Codarcea et al. (1961), Năstăseanu et al. (1981), Săndulescu (1984), Săndulescu and Dimitrescu (2004), and Mutihac (1990). The first to apply the global tectonics concepts for the Romanian Carpathians were Rădulescu and Săndulescu (1973).
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The South Carpathians represent an intricate pile of tectonic nappes, overthrusted from west eastwards during the Austrian (Middle Cretaceous) and Laramian paroxysmal phases, corresponding to various plate fragments. The napes are (from west eastwards): the Supragetic, Getic, Severin and Danubian
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The Supragetic, Getic Nappes as well as the Danubian Units represent units with both a metamorphic basement and a sedimentary cover, while the Severin Nappe includes only a sedimentary sequence. The Getic Nappe and the Danubian Units sediments include a
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sequence (Lowermost Jurassic – Middle Cretaceous). The Supragetic Nappe comprises mainly metamorphosed rocks (gneisses, micashists), while the Severin Nappe includes only Upper Jurassic – Lower Cretaceous sediments.
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Comănescu, Laura, & Alexandru Nedelea. 2016. Geomorphosites Assessments of the Glacial and Periglacial Landforms from Southern Carpathoans. In: Maria Radoane & Alfred Vespremeanu-Stroe (eds.),
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Năstăseanu, S., Bercia, I., Iancu, V., Vlad and Hârtopanu, I., 1981. The structure of the South Carpathians (Mehedinți – Banat Area). Guidebooks series, 22. IGR, Bucuresti, 3–100 pp.
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Codarcea, A., Răileanu, G., Pavelescu, L., Gherasi, N., Năstăseanu, S., Bercia, I. and Mercus, D., 1961. Guide des excursions. Carpates Meridionales, București, 130 pp.
339:, they are classified as having an alpine landscape. Their high mountain character, combined with great accessibility, makes them popular with tourists and scientists. 451: 1554: 1574: 1559: 83: 639: 515: 1399: 389:
Despite the heights, some of the most accessible passages in the Carpathians in Romania are along the rivers, which cross the mountain range (the
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Rădulescu, D. and Săndulescu, M., 1973. The plate-tectonics concept and the geological structure of the Carpathians. Tectonophysics, 16: 155–161.
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Codarcea , A., 1940. Vues nouvelles sur la tectonique du Banat meridional et du Plateau de Mehedinți. D. S. Inst. Geol. Rom., 20: 1–74.
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Murgoci, G.M., 1905. Sur l'existence d'une grande nappe de recouvrement dans les Carpathes meridionales. C. R. Acad. Sci., 7: 31.
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Săndulescu, M. and Dimitrescu, R., 2004. Geological structure of the Romanian Carpathians, Florence, 48 pp.
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The Southern Carpathians are the second highest group of mountains in the Carpathian Mountain range (after
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The first two groups are steepest on the North side, and the last two are steepest on the South side.
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Mutihac, V., 1990. Structura geologică a teritoriului României. Editura Tehnică, Bucharest, 419 pp.
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Moldoveanu peak (2544 m) is the highest in Romania and one of the highest peaks of the Carpathians
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From east to west, four mountain groups can be identified, separated by different river valleys.
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Săndulescu, M., 1984. Geotectonica României. Editura Tehnică, București, 336 pp.
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Earth's Landscape: An Encyclopedia of the World's Geographic Features
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Rivers in the west. To the south they are bounded by the
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Pictures and landscapes from the Southern Carpathians
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sequence (Upper Carboniferous, Lower Permian) and a
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Cham: Springer, p. 202. 924:Glacial lakes in the Retezat Mountains 828:Regular footpath in Făgăraș Mountains 588:; literally: "Mountains of the Skull") 578:; literally: "Mountains of the Thief") 1184: 684:Bucegi as seen from Postavaru massif 443:Lake Bucura in the Retezat Mountains 768:Jepii Mici Peak in Bucegi Mountains 13: 1616:Mountain ranges of the Carpathians 972:Waterfall in Retezat National Park 426: 393:) or form wide valleys (along the 358:, 2,535 metres – Făgăraș Mountains 14: 1637: 1169: 47:Peak 2,535 metres (8,317 ft) 1329: 977: 965: 953: 941: 929: 917: 912:One of many Parâng glacial lakes 905: 893: 881: 869: 857: 845: 833: 821: 809: 797: 785: 773: 761: 749: 737: 732:Scara summit in Bucegi Mountains 725: 713: 701: 689: 677: 201: 121: 38: 1539:Outer Subcarpathian depressions 1447:Retezat-Godeanu Mountains group 1410:Moldavian-Muntenian Carpathians 1141: 1132: 1123: 864:Piatra Craiului ridge in winter 780:Lake Bâlea in Făgăraș Mountains 606:; literally: "Hewed Mountains") 594:Retezat-Godeanu Mountains group 474:(literally: "Rock of the King") 1114: 1105: 1096: 1087: 1078: 1069: 1051: 1038: 1025: 696:Caraiman Cross on mountain top 656:; literally: "Pen Mountains"). 1: 1018: 876:Landscape in Parâng Mountains 291:. They cover the part of the 1457:Western Romanian Carpathians 1288:Central Moravian Carpathians 1214:, Groups, and Ranges of the 1001:Divisions of the Carpathians 960:Salvamont shelter in Retezat 708:Coștila 400 meters high wall 71:2,544 m (8,346 ft) 7: 1293:Slovak-Moravian Carpathians 989: 936:Bucura Peak in the distance 900:Shelter in Parâng mountains 10: 1642: 1606:Mountain ranges of Romania 1390:Central Beskidian Piedmont 1367:Căliman-Harghita Mountains 1298:Western Beskidian Piedmont 1283:South-Moravian Carpathians 1008:, at the South-Western end 816:Transfăgărășan alpine road 670: 454:– between the Prahova and 404: 314: 1626:Geography of Transylvania 1611:Mountain ranges of Serbia 1547: 1521: 1483: 1455: 1422: 1380: 1372:Giurgeu-Brașov Depression 1347: 1338: 1327: 1273: 1265:North Hungarian Mountains 1256:Lučenec-Košice Depression 1231: 1222: 756:Piatra Craiului Mountains 170: 160: 155: 141: 133: 119: 114: 75: 65: 57: 52: 37: 26: 21: 1251:Slovak Central Mountains 792:Challenging hiking trail 327:in the Făgăraș Mountains 1437:Făgăraș Mountains group 490:Făgăraș Mountains group 342:The highest peaks are: 1470:Poiana Ruscă Mountains 1442:Parâng Mountains group 948:Sunset on Retezat Peak 662:Poiana Ruscă Mountains 528:Parâng Mountains group 452:Bucegi Mountains group 444: 436: 328: 280: 198: 31: 1580:Ukrainian Carpathians 1555:Hungarian Carpathians 1529:Transylvanian Plateau 888:Parâng alpine scenery 442: 434: 322: 309:Balkan mountain range 1601:Southern Carpathians 1565:Romanian Carpathians 1424:Southern Carpathians 1241:Slovak Ore Mountains 1216:Carpathian Mountains 1014:, at the Eastern end 996:Romanian Carpathians 744:The Sphinx of Bucegi 397:Valley or along the 299:in the east and the 295:located between the 293:Carpathian Mountains 287:located in southern 199:Carpații Meridionali 187:Southern Carpathians 32:Carpații Meridionali 22:Southern Carpathians 1621:Geography of Europe 1570:Serbian Carpathians 1548:Grouping by country 1533:Transylvanian Plain 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Index

Romanian

Negoiu
Elevation
Coordinates
45°30′N 24°15′E / 45.500°N 24.250°E / 45.500; 24.250

Parent range
Carpathians
Orogeny
Age of rock
Triassic
Romanian
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