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Barotse Floodplain

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882: 66: 632:. Originally intended to be completed in 2006, it has been delayed by the difficulty of building on the floodplain. There is no rock in the region, and the causeway has been built from sand and gravel scooped out from shallow depressions next to it. Higher than usual floods washed away large sections. The contractor was a 311:
harder rock is found at the surface and has resisted the river's tendency to cut a channel down into it, and so acts a bit like a dam. Behind it the floodplain has formed. Below the falls the river falls nearly twice as fast as it does on the plain, and flows more swiftly in a narrower valley less
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occurs on the floodplain about 3 months after the peak of the rainy season in January–February. The flood usually peaks in April, and recedes in May to July, when grasses quickly grow on the exposed plain. At the river's lowest water in November the floodplain still contains about 537 km of
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In the occasional very wet year such as 2005, lives and property are lost in floods on the Barotse Plain. More often, however, it is a very good example of the principle that natural annual flooding by rivers is valuable and productive for wildlife and human populations, while damming rivers to
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November to January are lean months. Stored produce from the previous growing season is almost used up and in any case would need to be transported during the migration, while the new season's crops and grasses are not yet productive, and at the same time fishing stops for the spawning season.
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The satellite photo was taken in April 2004 at the peak of the flood, Note that the northern part of the plain, near Lukulu, is less flooded, the land there varies a bit more in height and the water tends to keep to the many river channels.
335:, principal town of the plain, situated at its edge. The main body of the plain covers about 5500 km, but the maximum flooded area is 10 750 km when the floodplains of several tributaries are taken into account, such as the 536:
The floodplain determines and dominates the way of life, economy, society and culture of the Lozi, who are skilled boat-builders, paddlers and swimmers. The annual migration with the flood is celebrated in the
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reported that the company underestimated the floodplain environment, and abandoned the contract. Subsequent modifications have been made to raise the road height and to increase the number and size of
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from vegetation killed by the initial flood, and from decaying aquatic plants left to dry out in the mud. It provides a good soil, but in the late dry season it bakes hard in the heat of the sun.
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Hunting and trapping animals, which might have filled the gap, is no longer available to most people, and trapping waterbirds is one of the few alternatives to buying flour.
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Tight control over access to the floodplain by the Litunga and the homogeneity of the indigenous people have slowed commercial development by outsiders.
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to grasslands at the edge of the floodplain when the flood arrives. The floodplain is one of the most productive areas for raising cattle in the country.
650:(AVIC International), finished the 286.9 million US dollars project. The road stretches 34 Kilometres in the Baroste plains with 26 bridges across it. 624:, via the ferry across the main river channel at Sandaula, which would then be replaced by a 500-metre bridge. It is treated as an extension of the 952: 937: 731: 709: 659: 647: 195: 977: 804: 413: 409: 402: 494:
The Lozi also catch fish, eating about five times as much as the national average. At the height of the flood they use
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system, which differs in having a large permanent lake and swamps, and a much smaller area which dries out annually.
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in the 19th century. In addition the entire western of the Zambezi within the country is a Game Management Area.
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and channels. The flood leaves behind a fertile grey to black soil overlaying the Kalahari sands, enriched by
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CIFA Occas.Pap., (7): 69 p. Published by Food and Agricultural Organization of the United Nations, Rome.
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rise on the higher ground to the north, which enjoys good rainfall (1400 mm annually) in a
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at an elevation of about 1000 m tilting very slightly to the south. The Zambezi and its
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ceremony held at Mongu, capital of Barotseland and its successor, the Western Province.
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in the north, to a point about 230 km south, above the Ngonye falls and south of
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from October to May. A flood moves down the river reaching a flat region, formed from
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to connect a small harbour at Mongu to the Zambezi's channel in the dry season
926: 908: 895: 771:"Barotse Floodplain, Zambia: local economic dependence on wetland resources." 582: 320: 90: 522: 488: 440: 339:. The Barotse Floodplain is the second largest wetland in Zambia after the 308: 300: 296: 172: 105: 77:
The Zambezi flowing north to south through the middle of the floodplain;
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About 250,000 people live on the plain with a similar number of cattle,
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Cuando river and floodplain, on the border between Angola and Zambia;
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sands, about five hundred kilometres across. To the south around the
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As the floods recede, water is left behind in lagoons, swamps, and
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a broad floodplain which carries overspill from high floods of the
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across the centre of the floodplain to take a paved highway from
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Welcomme, R.L. (Comp.) (1979): ”The inland fisheries of Africa."
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Development on the plain has been restricted until now to—
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just before the flood, the first floodwaters are naturally
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Sylvia Mweetwa: "Road financiers to extend agreement."
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in the lagoons left behind by the falling flood. Fish
513:The Lozi cultivate crops on the floodplain such as 73:as the bright green to dark blue central region. 924: 249:, regarded as being of high conservation value. 256:as spawning the culture and way of life of the 595: 588:some intensive rice and sugarcane plantations. 549:, is potentially damaging to the environment. 729:"Zambezi Floodplain Ramsar Information Sheet" 482: 602:Lusaka–Mongu Road § Westwards extension 315:The floodplain stretches from the Zambezi's 137:swamps and floodplain of the Lungwebungu; 350: 545:control floods, as has happened with the 133:, seat of the Litunga during the flood; 93:, marking the start of the floodplain; 64: 707:"Seasonal Flooding in Southern Africa". 925: 858:online at www.zambia-travel-guide.com. 766: 764: 762: 760: 758: 756: 754: 752: 660:List of crossings of the Zambezi River 648:Aviation Industry Corporation of China 396: 286: 69:NASA satellite photograph showing the 953:Geography of Western Province, Zambia 784: 782: 576:constructed on mounds, such as Lealui 498:and spears for fishing, and they use 443:, waterbirds, fish-eating birds, and 877:Terracarta/International Travel Maps 774:Case Studies in Wetland Valuation #2 749: 167:Lui River with narrow floodplain; 13: 887:online retrieved 19 November 2007. 875:"Zambia 1:1,500,000 2nd Edition", 779: 382:deposited by the flood as well as 81:confluence of (left to right) the 16:Major floodplain in Central Africa 14: 994: 196:Central Zambezian Miombo woodland 812:Consolidated Contractors Company 740:Ramsar Sites Information Service 938:Flooded grasslands and savannas 585:at Sandaula, Libonda and Lukulu 97:end of the floodplain south of 856:Zambia: The Bradt Travel Guide 847: 833: 817: 794: 722: 700: 672: 552: 141:the Kabompo drains an area of 1: 746:. Retrieved 22 November 2007. 665: 260:, "Rotse" being a variant of 978:Zambezian flooded grasslands 414:Zambezian Baikiaea woodlands 410:Western Zambezian grasslands 403:Zambezian flooded grasslands 198:west of Mongu features many 7: 860:Retrieved 21 November 2007. 653: 596:Barotse Floodplain causeway 115:, capital of Barotseland; 10: 999: 599: 483:Human ecology of the plain 207:Sioma Ngwezi National Park 801:Bulletin 74 (August 2004) 687:Sites Information Service 473:Liuwa Plain National Park 420:) in the north and east. 418:Cryptosepalum dry forests 412:) with woodland savanna ( 401:The floodplain is in the 229:is one of Africa's great 188:Liuwa Plain National Park 59: 51: 43: 35: 26: 21: 463:and small antelope such 252:The name recognises the 143:Cryptosepalum dry forest 884:MSN Encarta World Atlas 854:Chris McIntyre (2004). 807:March 26, 2009, at the 734:March 26, 2009, at the 579:a few dry season tracks 351:Flood levels and timing 968:Ramsar sites in Zambia 744:Wetlands International 210: 983:Floodplains of Africa 680:"Zambezi Floodplains" 291:The region is a flat 245:. It is a designated 68: 943:Ecoregions of Africa 272:under their king or 126:on the floodplain; 85:, Southern Kashiji, 963:Geography of Zambia 905: /  606:A new project, the 572:small villages and 423:The flood provides 397:Natural environment 312:prone to flooding. 287:Topography and area 227:Zambezi Floodplain, 215:Barotse Floodplain, 39:Zambezi Floodplains 958:Wetlands of Zambia 933:Barotse Floodplain 879:, Vancouver, 2000. 717:NASA/Visible Earth 712:2008-09-23 at the 325:Lungwebungu Rivers 217:also known as the 211: 71:Barotse Floodplain 52:Reference no. 909:15.033°S 22.883°E 776:: IUCN, May 2003. 626:Lusaka-Mongu Road 609:Mongu-Kalabo road 427:for fish such as 359:Climate of Zambia 108:on the Zambezi; 63: 62: 990: 920: 919: 917: 916: 915: 910: 906: 903: 902: 901: 898: 861: 851: 845: 844: 837: 831: 821: 815: 798: 792: 786: 777: 768: 747: 726: 720: 704: 698: 697: 695: 693: 676: 425:aquatic habitats 365:The peak of the 239:Western Province 159:floodplain near 19: 18: 998: 997: 993: 992: 991: 989: 988: 987: 923: 922: 914:-15.033; 22.883 913: 911: 907: 904: 899: 896: 894: 892: 891: 865: 864: 852: 848: 839: 838: 834: 830:, 5 April 2007. 828:Times of Zambia 822: 818: 809:Wayback Machine 799: 795: 787: 780: 769: 750: 736:Wayback Machine 727: 723: 714:Wayback Machine 705: 701: 691: 689: 678: 677: 673: 668: 656: 639:Times of Zambia 604: 598: 583:pontoon ferries 555: 485: 399: 353: 289: 270:Southern Africa 194:The flat sandy 157:Luanginga River 47:2 February 2007 31: 17: 12: 11: 5: 996: 986: 985: 980: 975: 970: 965: 960: 955: 950: 945: 940: 935: 889: 888: 880: 872: 871: 869:Map references 863: 862: 846: 832: 816: 793: 778: 748: 721: 699: 670: 669: 667: 664: 663: 662: 655: 652: 597: 594: 590: 589: 586: 580: 577: 570: 567:colonial times 554: 551: 484: 481: 398: 395: 363: 362: 352: 349: 341:Lake Bangweulu 288: 285: 152:(floodplain); 122:, seat of the 91:Kabompo Rivers 61: 60: 57: 56: 53: 49: 48: 45: 41: 40: 37: 33: 32: 29:Ramsar Wetland 27: 24: 23: 15: 9: 6: 4: 3: 2: 995: 984: 981: 979: 976: 974: 973:Zambezi River 971: 969: 966: 964: 961: 959: 956: 954: 951: 949: 946: 944: 941: 939: 936: 934: 931: 930: 928: 921: 918: 886: 885: 881: 878: 874: 873: 870: 867: 866: 859: 857: 850: 842: 836: 829: 825: 820: 813: 810: 806: 802: 797: 790: 785: 783: 775: 772: 767: 765: 763: 761: 759: 757: 755: 753: 745: 741: 737: 733: 730: 725: 718: 715: 711: 708: 703: 688: 686: 681: 675: 671: 661: 658: 657: 651: 649: 645: 641: 640: 635: 631: 627: 623: 619: 615: 611: 610: 603: 593: 587: 584: 581: 578: 575: 571: 568: 564: 560: 559: 558: 550: 548: 542: 540: 534: 530: 528: 524: 520: 516: 511: 509: 505: 501: 497: 492: 490: 480: 478: 474: 470: 466: 462: 458: 454: 450: 447:, the wading 446: 442: 438: 434: 430: 426: 421: 419: 415: 411: 407: 404: 394: 392: 387: 385: 381: 377: 373: 368: 361: 360: 355: 354: 348: 344: 342: 338: 334: 330: 326: 322: 318: 313: 310: 306: 302: 298: 294: 284: 282: 278: 275: 271: 267: 263: 259: 255: 250: 248: 244: 240: 236: 235:Zambezi River 232: 228: 224: 220: 216: 208: 205: 201: 197: 193: 189: 186: 182: 178: 174: 170: 166: 162: 158: 155: 151: 148: 144: 140: 136: 132: 129: 125: 121: 118: 114: 111: 107: 104: 100: 96: 92: 88: 84: 80: 76: 72: 67: 58: 54: 50: 46: 42: 38: 36:Official name 34: 30: 25: 20: 890: 883: 876: 868: 855: 849: 835: 827: 819: 796: 773: 739: 724: 716: 702: 690:. Retrieved 683: 674: 637: 607: 605: 591: 556: 543: 535: 531: 523:sweet potato 512: 493: 486: 441:hippopotamus 422: 400: 388: 364: 356: 345: 314: 309:Ngonye Falls 301:rainy season 290: 261: 251: 226: 222: 219:Bulozi Plain 218: 214: 212: 203: 191: 184: 180: 173:Cuando River 168: 164: 153: 146: 138: 134: 127: 116: 109: 106:Ngonye Falls 102: 94: 78: 74: 70: 22:Designations 948:Barotseland 912: / 553:Development 547:Kafue Flats 391:oxbow lakes 337:Luena Flats 281:Barotseland 258:Lozi people 247:Ramsar site 150:Luena Flats 83:Lungwebungu 927:Categories 814:of Kuwait. 666:References 600:See also: 527:sugar cane 496:fish traps 453:wildebeest 437:crocodiles 317:confluence 297:headwaters 254:floodplain 44:Designated 574:compounds 500:gill nets 489:migrating 429:tigerfish 406:ecoregion 357:See also 319:with the 233:, on the 131:Limulunga 805:Archived 732:Archived 710:Archived 692:25 April 654:See also 644:culverts 614:causeway 539:Kuomboka 477:Lewanika 469:steenbok 461:tsessebe 449:antelope 305:Kalahari 277:Lewanika 231:wetlands 900:22°53′E 826:Ndola: 565:dug in 508:hypoxic 372:lagoons 329:Senanga 321:Kabompo 293:plateau 274:litunga 266:Central 237:in the 225:or the 124:Litunga 99:Senanga 87:Zambezi 897:15°2′S 685:Ramsar 634:Kuwait 630:Lusaka 622:Kalabo 525:, and 445:lechwe 376:swamps 243:Zambia 223:Lyondo 177:Angola 161:Kalabo 120:Lealui 738:, in 628:from 618:Mongu 563:canal 515:maize 504:spawn 465:oribi 457:zebra 433:bream 384:humus 367:flood 333:Mongu 113:Mongu 694:2018 561:the 519:rice 467:and 431:and 380:silt 323:and 262:Lozi 213:The 200:pans 89:and 55:1662 620:to 241:of 175:in 163:; 145:; 929:: 803:, 781:^ 751:^ 742:, 682:. 529:. 521:, 517:, 459:, 455:, 439:, 435:, 393:. 374:, 283:. 221:, 204:17 202:; 192:16 190:; 185:15 181:14 179:; 169:13 165:12 154:11 147:10 139:9 135:8 128:7 117:6 110:5 103:4 101:; 95:3 79:2 843:. 696:. 268:/ 209:. 75:1

Index

Ramsar Wetland

Lungwebungu
Zambezi
Kabompo Rivers
Senanga
Ngonye Falls
Mongu
Lealui
Litunga
Limulunga
Cryptosepalum dry forest
Luena Flats
Luanginga River
Kalabo
Cuando River
Angola
Liuwa Plain National Park
Central Zambezian Miombo woodland
pans
Sioma Ngwezi National Park
wetlands
Zambezi River
Western Province
Zambia
Ramsar site
floodplain
Lozi people
Central
Southern Africa

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