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Nafusa Mountains

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118: 111: 318:(1,100 ft) of topographic prominence. A series of deep valleys which drain north toward the Jefara cut into this escarpment. It extends about 250 km (160 mi) within Libya, from just east of the city of Gharyan (about 60 km (40 mi) south of Tripoli) in the east to the city of Wazzin at the Tunisian border in the west. Spurs and isolated upthrusts continue into Tunisia, but this region is almost unpopulated, in marked contrast to the situation in Libya. 283:). In the aftermath, citing them as heretics, Ibrahim II executed all the Nafusa prisoners and put an end to their independent imamate (Tahert fell shortly after, in 911). Despite the destruction of their states, Ibadi Islam remained a strong (if clandestine) faith among the Berbers of the Nafusa mountains for centuries after, down to the modern day. The lingering heterodoxy of the Nafusa people has placed them frequently at odds, or under suspicion, by the largely orthodox 299:, when their initiatives led to the Nafusa Mountains becoming a major front in that war. The terrain and topography of the region are critical strategic factors, constraining mechanised advances from the flat plain and plateau, and favouring guerrilla tactics based on close local knowledge and the advantage of high ground. By the end of June 2011 the Nafusi people had almost succeeded in liberating themselves completely from the control of the regime. 783: 382: 38: 859: 405:
border crossing was captured and held to ensure supply lines from Tunisia; all the mountain towns were retaken; and the front extended to the plains, cutting regime communications lines and allowing electricity to be restored. They were the first rebel combatants to be supplied with arms by air-drop.
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The mountain area is rarely more than 25 km (16 mi) in depth, from its southern boundary, the flat arid plateau some 650 m (2,100 ft) above sea level, to its northern limit on the plain, where the land falls to below 150 m (490 ft). Much of the 500 m (2,000 ft)
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The Nafusa Mountains became first a hotbed for anti-Gaddafi protests (with protests breaking out relatively early in Nalut and Zintan) and then a rebel stronghold, an island of rebel control in the mainly Gaddafi-controlled western part of the country. During the early stages, forces allied to the
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of the Tripolitanian Plateau slope downwards to the south and tilt upwards towards the north creating the highest portion of the plateau as the Nafusa mountains which rise to over 750 m (2,500 ft). The plateau ends abruptly on the north with an escarpment which has up to 350 m
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may be up to 350 m (1,100 ft). It is from below, on the plain, viewing the steep slopes and sharply-etched skyline that the area appears mountainous; from the plateau the land appears merely hilly, and in fact it is rather flat apart from the effects of differential erosion.
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took refuge in the Nafusa Mountains. Preachers converted and organized the native Nafusa people into a fighting force. Under the leadership of Imam Abu al-Khattab al-Ma'afari, the Nafusa descended from the mountains and proceeded to conquer all of the crumbling
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In the course of the civil war, many towns in the area were subjected to shelling by artillery and rockets from both sides, with much damage to infrastructure. Regime forces cut off electricity and water supplies.
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in 761 (his third attempt - his first two armies had been repulsed) and put an end to their putative new state. However, the Nafusa mountains themselves remained unconquered. Throughout the 9th century, while the
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of Egypt invaded Aghlabid Ifriqya and captured Tripoli. But the Nafusa challenged and destroyed the Egyptian army in 880. Again the Nafusa victory was short-lived. In 896-97, the Aghlabid emir
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Asketell, J. M. and Ghellali, S. M. (1991) "A palaeogeologic map of the pre-Tertiary surface in the region of the Jifarah Plain: its implication to the structural history of Northern Libya"
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ruled in Ifriqiya, the Ibadi maintained an independent puritan republic in the Nafusa mountains. The Imamate of Nafusa was in close alliance with the other Ibadi remnant, the
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The Nafusa Mountains form the boundary between the Libyan coastal plain, known as the Jafara, to the north, and the Tripolitanian Plateau to the south. The
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El-Zouki, Ashour V. (1980) "Stratigraphy and lithofacies of the continental clastic (Upper Jurassic and Lower Cretaceous) of Jabal Nafusah, NW Libya"
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Ethic composition of the Libyan population in 1974. The orange arc in the Northwest shows the Berber population in the Nafusa Mountains.
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culture and language, after four decades during which there were severe punishments for speaking and writing Tamazight openly.
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in early summer 2011, and while fierce fighting continued, Berber exhibitions and workshops sprang up to share and spread the
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The geology of Libya. Volume IV–VII : Third Symposium on the Geology of Libya, held at Tripoli, September 27–30, 1987
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This distinct culture, suppressed and oppressed by the Libyan regime, has risen to new prominence in the course of the
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As towns and villages in the Nafusa Mountains and surrounding areas were liberated from control by forces loyal to
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was without electricity and water for seven weeks, and more than 45,000 refugees fled for safety to the adjoining
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Megerisi, Mohamed and Mamgain, V. D. (1980) "The Upper Cretaceous-Tertiary formations of northern Libya"
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The mountain villages raise primarily goats, olives and grain, but also have fig and apricot orchards.
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national transitional government succeeded in evacuating most non-combatants into Tunisia; the
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recovered Tripolitana and defeated the Nafusa in a great battle at Manu (south of
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Arab governor of Egypt invaded Ifriqya, defeated the Nafusa in a battle at
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drop in level is accomplished abruptly, at the escarpment, where local
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The area was a major population and cultural center of the
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Histoire de l'Afrique du Nord, de la conquete Arabe à 1830
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The Geology of Libya: Symposium on the Geology of Libya
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The Geology of Libya: Symposium on the Geology of Libya
745:"Nafusa Mountains: Winding roads, rugged mountains" 693:. Tunisian News Agency. 21 May 2011. Archived from 476:
Tripolitanien, Syrtebogen, Fezzan und die Kyrenaika
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DuMont Reiserverlag. p. 14. 164: 28: 13: 14: 902: 738: 611:Spencer, Richard (29 June 2011). 287:population of the rest of Libya. 857: 781: 213: 210:, who repeatedly expanded west. 116: 109: 36: 709: 683: 656: 330:Towns in the mountains include 663:Robertson, Nic (22 May 2011). 630: 604: 553: 525: 505: 492: 467: 396:2011 Nafusa Mountains Campaign 218:In the aftermath of the great 1: 716:Simpson, John (5 July 2011). 461: 474:Willeitner, Joachim (2001). 430:, where many had relatives. 302: 7: 449: 10: 907: 393: 373: 306: 201: 55:975 m (3,199 ft) 853: 795: 669:CNN International Edition 139: 103: 98: 59: 49: 44: 35: 26: 21: 886:Mountain ranges of Libya 412:Médecins Sans Frontières 364:Jabal al Gharbi District 324:topographic prominences 297:Libyan Civil War (2011) 175:region of northwestern 386: 277:Ibrahim II of Ifriqiya 390:2011 Libyan civil war 384: 291:2011 Libyan civil war 671:. Cable News Network 498:C.A. Julien, (1931) 434:Cultural renaissance 222:of the 8th century, 511:Julien (1931: p.39) 83:31.8649°N 11.7933°E 79: /  456:Cave dwelling Jews 387: 309:Geography of Libya 45:Highest point 16:Mountains in Libya 873: 872: 228:Umayyad Caliphate 153: 152: 130:Location in Libya 898: 861: 860: 786: 785: 774: 767: 760: 751: 750: 733: 732: 730: 728: 713: 707: 706: 704: 702: 687: 681: 680: 678: 676: 660: 654: 653: 651: 649: 644:on 23 March 2012 634: 628: 627: 625: 623: 608: 602: 584: 575: 557: 551: 529: 523: 518: 512: 509: 503: 496: 490: 489: 471: 262:Rustamid dynasty 247:in 758. But the 166: 157:Nafusa Mountains 124:Nafusa Mountains 120: 119: 113: 94: 93: 91: 90: 89: 88:31.8649; 11.7933 84: 80: 77: 76: 75: 72: 40: 31: 30: 22:Nafusa Mountains 19: 18: 906: 905: 901: 900: 899: 897: 896: 895: 876: 875: 874: 869: 849: 791: 780: 778: 741: 736: 726: 724: 714: 710: 700: 698: 689: 688: 684: 674: 672: 661: 657: 647: 645: 636: 635: 631: 621: 619: 609: 605: 585: 578: 558: 554: 530: 526: 519: 515: 510: 506: 497: 493: 486: 472: 468: 464: 452: 440:Muammar Gaddafi 436: 414:sent a team in 398: 392: 376: 311: 305: 293: 216: 204: 171:in the western 135: 134: 133: 132: 131: 128: 127: 126: 125: 121: 87: 85: 81: 78: 73: 70: 68: 66: 65: 17: 12: 11: 5: 904: 894: 893: 888: 871: 870: 868: 867: 854: 851: 850: 848: 847: 842: 837: 832: 827: 822: 817: 812: 807: 802: 796: 793: 792: 777: 776: 769: 762: 754: 748: 747: 740: 739:External links 737: 735: 734: 708: 697:on 25 May 2011 682: 655: 629: 603: 576: 552: 535:Salime, M. J. 524: 513: 504: 491: 484: 465: 463: 460: 459: 458: 451: 448: 435: 432: 394:Main article: 391: 388: 375: 372: 368:Nalut District 304: 301: 292: 289: 215: 212: 203: 200: 169:mountain range 151: 150: 141: 137: 136: 129: 123: 122: 115: 114: 108: 107: 106: 105: 104: 101: 100: 96: 95: 63: 57: 56: 53: 47: 46: 42: 41: 33: 32: 24: 23: 15: 9: 6: 4: 3: 2: 903: 892: 889: 887: 884: 883: 881: 866: 865: 856: 855: 852: 846: 843: 841: 838: 836: 833: 831: 828: 826: 823: 821: 818: 816: 813: 811: 808: 806: 803: 801: 798: 797: 794: 790: 787:Mountains of 784: 775: 770: 768: 763: 761: 756: 755: 752: 746: 743: 742: 723: 719: 712: 696: 692: 686: 670: 666: 659: 643: 639: 633: 618: 617:The Telegraph 614: 607: 601: 600:0-12-615501-1 597: 593: 589: 583: 581: 574: 573:0-12-615501-1 570: 566: 562: 556: 550: 549:0-444-88844-6 546: 542: 539:(ed.) (1991) 538: 534: 528: 522: 517: 508: 501: 495: 487: 485:3-7701-4876-2 481: 477: 470: 466: 457: 454: 453: 447: 445: 441: 431: 429: 425: 421: 417: 413: 407: 404: 397: 383: 379: 371: 369: 365: 361: 357: 353: 349: 345: 341: 337: 333: 328: 325: 319: 316: 315:beds (strata) 310: 300: 298: 288: 286: 282: 278: 274: 269: 267: 263: 259: 254: 250: 246: 242: 238: 234: 229: 225: 221: 220:Berber Revolt 214:Ibadi imamate 211: 209: 199: 197: 193: 192:coastal plain 190: 189:Mediterranean 186: 182: 178: 174: 170: 162: 158: 149: 145: 142: 138: 112: 102: 97: 92: 64: 62: 58: 54: 52: 48: 43: 39: 34: 25: 20: 891:Tripolitania 863: 845:Waw an Namus 829: 825:Jebel Akhdar 725:. Retrieved 721: 711: 699:. Retrieved 695:the original 685: 673:. Retrieved 668: 658: 646:. Retrieved 642:the original 632: 620:. 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Index


Elevation
Coordinates
31°51′54″N 11°47′36″E / 31.8649°N 11.7933°E / 31.8649; 11.7933
Nafusa Mountains is located in Libya
Tripolitania
Libya
Arabic
mountain range
Tripolitania
Libya
escarpment
Plateau
Mediterranean
coastal plain
Libu
Berber Revolt
Ibadi
Umayyad Caliphate
Fihrid
Ifriqiya
Tripoli
Kairouan
Abbasid
Tawergha
Aghlabids
Rustamid dynasty
Tiaret
Tulunids
Ibrahim II of Ifriqiya

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