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Lake Débo

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313:." The flat slopes and geology of the beds has resulted in creating a meandering and multi-channel flow pattern, which has resulted in the formation of inner delta of the Niger. The inner delta thus has many wide channels, which are shallow and flooded marshes; this delta extends over a length of 320 km (200 mi) with a width of 80 km (50 mi). It is inferred from the study of nearly 400 maps that it is the delta which is the origin of the lake and that the lake is the largest in the delta. It is integral to the wide river channel with its size fluctuating with variation of the water level in the lake. It also provides confirmation of the nature of blocked water and also includes the 345:, just south of the Sahara desert, has climatic conditions which are reported to be a transitional zone of humid Guinean climate in the south to a dry climate at border with the Sahara. The rainy season in the south lasts from July to October, with an average annual rainfall of 750 mm (30 in). However, the rainy season in the north lasts from July to September, with an average annual precipitation recorded at 250 mm (9.8 in). Temperatures vary with strong seasonal emphasis. The average maximum temperature recorded in May at 45: 527: 29: 186:. During high water stages of the river, the delta formed by lakes, creeks, and backwaters form part of Lake Débo. The inner delta has many wide channels, which are shallow and flooded marshes; this delta extends over a length of 320 kilometres (200 miles) with a width of 80 km (50 mi). Lake Débo during high flow season, is at a distance of 80 km (50 mi) from Mopti on its upstream, on the southern end and 240 km (150 mi) from 1410: 478: 374: 219: 321:
during November and December. The lake has a vast expanse of water extending on all sides. The river that is formed at the outlet of the lake has a width of 10 km (6 mi) for a length of 10 km (6 mi) downstream, where after it narrows down, gets spilled into many channels; marshy islands are formed and depth of water is in the range of 2.4–3.0 m (8–10 ft). Foolahs, the
629: 263: 52: 254:. The lake has been known variously as Nigrite Palus, Lake Sigisma, Lake Guber, Lake Guarda, Bog/Morais of Guarda, Lake Maberia, Bahar Seafeena, Lake Dibbie, but it is now known as Lake Débo. The Niger River is assessed as a young river of 2000 years age and is yet to stabilize. However, the natural channels have undergone many meandering changes. 279:
before the creation of the lake is 1.5 m (5 ft) per 160 km (100 mi). The lake is divided by a barrier into two zones, the upper and the lower. The barrier extends several kilometres southwards. Beyond the barrier, the lake is narrow and long and its outreach is not visible. The Bara Lisa River joins the Niger above
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lake in Mali, which has diameter of 30 km (19 mi) and shallow and hence large vessels can not pass through the lake. In the upper highland reaches of these rivers, the highland terrain slopes are very gentle resulting in the retardation of flows and creation of this lake. The slope reported
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Below Lake Debo, the Niger valley is marked by a large number of lakes, which are lower than the river level. As part of the central delta, the lake is the largest. As it is a part of the Niger River, its size varies with the fluctuation in the water level. and maximum flood occurs in the river
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During the high flood stage, flood waters arriving at the lake are reported as 12,400 km/s (178,000 cu mi/min). This was absorbed in the vast lake, as storage, and the out flow from the lake is thus moderated to only 2,400 km/s (35,000 cu mi/min) when it reaches
333:, the capital city of Niger. Since 1962, even a 1,000 km/s (14,000 cu mi/min) extra flow from the lake could now cause increase of water level in the Niamey area by 2 m (6 ft 7 in), rising to the level 181.51 metres (595 ft 6 in). 464:
The sloping banks of the lake have shrubs interspersed with grasses and vacant patches, and woody species, generally of acacia species. Akkagoun and Dentaka are the forested areas surrounding the lake and the delta, which are home for many water birds.
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is 40 °C (104 °F). The cooler climatic season is from December to January with temperatures dropping to a mean minimum of 3 °C (37 °F) to 6 °C (43 °F) in the northern part of the delta.
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Lake Débo during high flow season when it has the maximum dimensions of water spread, is 80 km (50 mi) from Mopti on its upstream, on the southern end, and 240 km (150 mi) from
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Michele L. Thieme; Robin Abell; Neil Burgess; Bernhard Lehner; Eric Dinerstein; David Olson; Guy Teugels; Andre Kamdem-Toham; Melanie L. J. S. Stiassny; Paul Skelton (5 April 2005).
250:. Study of more than 400 maps of the region created over a period from 1000 to 1900 AD found that the lake appeared on 95 percent; the only feature depicted on more maps was the 422:(the chief Joro); the "Harima" (meaning: a local convention) with the chief of village and other members responsible for its usage; and the several small holdings (within the 767: 194:, and the largest lake within Mali. Its size is largely reduced during the dry season of September to March. The existence of this lake called the "Great Lake" in the 393:(Inner Niger Delta in Mali) form the pasture lands which are collectively known as the flooded forest savannah with aquatic herbaceous and two dominant species of 1086:
Samuel Greatheed; Daniel Parken; Theophilus Williams; Thomas Price; Josiah Conder; William Hendry Stowell; Jonathan Edwards Ryland; Edwin Paxton Hood (1830).
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in Mali has been established after extensive study of maps of the region extending over a period from 1000 to 1900 AD; 400 maps were studied for the period.
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when the water stages in the lake and the delta is high. The aquatic plants sustain varying levels of water in the lake and the soil types dictates the
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The aquatic fauna in the delta as a whole, which is reflective of the lake also, consists of 130 species mostly of the species in the families of
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There are three types of pasture lands, defined on the basis of its management. These are: Resident Fulani's pastures which are controlled by the
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ecozones. Over one million birds have been recorded as using the lake;, including a large number of migratory and resident species, such as
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who live here, use these marshes as pastures in the dry season and thereafter they go back to their habitats in the interior of the basin.
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are dwindling. A sea side feeling is felt around the lake and the delta, as the air is filled with the sounds of water birds and
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is also reported from the flood plains. Within the basin area of the lake and the delta mammal species reported include:
667:. There are many migratory fish species which migrate along the river to this region; out of these migrating fishes the 426:) parceled to private individuals. the perennial grasses grown are edible and easily digestible with botanical names of 705:
fisherman, resident on the shores of the lake are involved in these operations. During the dry season, the many ethnic
438:, and which grow in varying depths of water (3–5 m or 10–16 ft). The crop variety, which is extensive, is of 361:
at its downstream, on the north-eastern end. It is the largest of many such seasonal wetlands and lakes which form the
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in Mali, was known to Europeans from very early times. The earliest known report of it was in the first millennium BC.
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at its downstream, on the north-eastern end. It is the largest of many such seasonal wetlands and lakes which form the
1654: 1455: 287:, the main arm of the lake, exits from the lake in a westerly direction and turns northeast to join the Bara Lisa. 44: 1737: 365:, and the largest lake within Mali. Its size is largely reduced during the dry season of September to March. 1680: 1659: 1241: 1624: 1349: 1148: 491:
is the most prominent fauna species in the lake which is reported as its last habitat in the world.
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are also reported from the lake (the hippo population is estimated at 40 to 60 individuals).
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are also reported from the lake which could result in reduction of the water transparency.
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Travels Through Central Africa to Timbuctoo and Across the Great Desert to Morocco 1824-28
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region. The maximum flood in the lake and the delta occurs during November and December.
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Gerald J. Rizzo (2006). "The Patterns and Meaning of a Great Lake in West Africa".
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are two endemic species of fishes in the lake which is part of the inland delta.
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nomads come to this lake area as their terminus destination during the seasonal
283:. It exits the deltas from the northern shores of Lake Debo and flows east. The 1521: 1466: 668: 563: 504: 496: 434: 137: 801: 1731: 1516: 1491: 1301: 1238:"Applied GIS for Managing Flooded Pastures of Lake Debo and Walado Debo/Mali" 526: 500: 92: 79: 954: 701:, fishing operations are carried out in the lake using trawlers. The ethnic 280: 28: 1506: 1496: 1486: 1429: 710: 579: 516: 508: 481: 306: 1603: 1531: 1511: 1444: 1424: 1365: 1031:
Freshwater Ecoregions of Africa and Madagascar: A Conservation Assessment
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found within the lake area, which forms one of the major wetlands in the
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Geological formations recorded at the bed of the lake are "from dense
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travels long distances up to the delta and also up to the toe of the
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Inner Niger Delta, including Lake Debo, flooded savanna ecoregion map
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Alive in the Writing: Crafting Ethnography in the Company of Chekhov
477: 235: 203: 1567: 672: 539: 373: 358: 310: 302: 239: 207: 187: 1557: 1634: 1587: 1547: 819:"Support Project for Wetland Management In the Inner Niger Delta" 458: 247: 243: 218: 1582: 1577: 1552: 614: 394: 330: 322: 1334: 1067:. Taylor & Francis. 1957. pp. 253–. GGKEY:XNB450PQT77 1562: 1114:
Bridge Over Niger: The True Story of the J. F. Kennedy Bridge
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The lake is formed upstream of the confluence of Niger and
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Ralph H. Hughes; Jane S. Hughes; G. M. Bernacsek (1992).
1149:"Case of Flooded Pasture in Lake Débo and Walado Débo, 1207:
Update 019 April 24th, Debo Lake --Sunny Water World
988: 1079: 738:"The Inland Niger Delta: A Cartographic Connection" 1023: 1021: 1019: 950: 948: 1110: 713:migration along with their herds from the north. 1729: 70: 1016: 945: 791: 768:"The Inland Niger Delta: A Cartographic Beacon" 609:As the lake is an important stopping place for 1296: 1294: 415:are also reported on the fringes of the lake. 1350: 1310:. University of Chicago Press. pp. 32–. 1300: 995:. Cambridge University Press. pp. 68–. 33:Mud houses on the center island at Lake Débo 1291: 1055: 982: 849: 765: 1357: 1343: 1232: 1230: 1228: 1104: 989:Roderick J. McIntosh (29 September 2005). 877: 546:, is represented by species from both the 226:This lake, called the "Great Lake" in the 1273:"Ecoregion Description:Inner Niger Delta" 1267: 1265: 1263: 1261: 1259: 917: 911: 843: 813: 811: 174:, formed by the seasonal flooding of the 1197: 1195: 1151:Journal Computer and Information Science 761: 759: 627: 525: 476: 372: 309:and covered by a hard layer of cemented- 261: 217: 1240:. Journal of GIS Trends. Archived from 1225: 921:Hydrology and Water Resources of Africa 883: 1730: 1256: 1143: 1141: 856:. Bradt Travel Guides. pp. 172–. 808: 770:. Afriterra Foundation. Archived from 732: 730: 728: 726: 397:. These pastures are known locally as 246:described it as having the shape of a 1338: 1192: 756: 1167: 1111:Remo Capra Bloise (11 August 2000). 1209:. Jinfeibao8844.com. Archived from 1138: 723: 349:is 43 °C (109 °F) and at 13: 958:Iucn Directory of African Wetlands 824:. Cmsdata.iucn.org. Archived from 14: 1759: 515:, whilst reptile species include 51: 1408: 301:compacted in the broad Taoudeni 157:160 km (62 sq mi) 50: 43: 27: 1364: 1034:. Island Press. pp. 187–. 850:Ross Velton (1 December 2004). 740:. Afriterra.org. Archived from 918:M. Shahin (30 November 2002). 785: 621:zone under the title whole of 1: 716: 368: 1681:National Park of Upper Niger 1660:River Niger Bridge (Onitsha) 389:The inundated Lake Débo and 257: 7: 1155:. Science Journal. May 2011 924:. Springer. pp. 307–. 890:. Routledge. pp. 21–. 10: 1764: 1117:. iUniverse. pp. 7–. 684: 336: 213: 1699: 1668: 1617: 1596: 1540: 1453: 1417: 1406: 1372: 802:10.1080/03085690500362439 432:(a perennial plant) and 222:Lake Débo seen from space 153: 149: 136: 122: 108: 69: 38: 26: 21: 884:Caillie (7 March 2013). 472: 1179:Encyclopædia Britannica 961:. IUCN. pp. 394–. 617:has classified it as a 588:white-winged black tern 274:. It is the best known 170:in the central part of 796:. 58 (Part 1): 80–89. 636: 535: 484: 386: 267: 223: 1676:Niger Basin Authority 631: 529: 480: 376: 265: 221: 1738:Ramsar sites in Mali 1717:Ogbaru boat disaster 1691:Kainji National Park 1203:"Africa adventure 4" 992:Ancient Middle Niger 489:West African manatee 453:Vetiveria nigritiana 444:Oryza longistaminata 429:Echinochloa stagnina 178:basin. It is in the 93:15.31667°N 4.10000°W 1712:Kwara boat disaster 1707:Kebbi boat disaster 1425:Source of the Niger 1304:(26 January 2012). 1089:The Eclectic Review 600:black crowned crane 596:black-tailed godwit 532:black-crowned crane 521:African rock python 513:red-fronted gazelle 89: /  1279:on 29 October 2013 1244:on 16 October 2011 831:on 24 October 2012 642:Synodontis gobroni 637: 536: 485: 412:Borassus aethiopum 403:grass. Palms like 387: 268: 224: 98:15.31667; -4.10000 1725: 1724: 1435:Inner Niger Delta 1317:978-0-226-56792-1 1124:978-1-4697-7432-9 1041:978-1-59726-791-5 1002:978-0-521-81300-6 968:978-2-88032-949-5 931:978-1-4020-0866-5 897:978-0-415-42792-0 863:978-1-84162-077-0 766:Gerald J. Rizzo. 576:great white egret 406:Hyphaene thebaica 363:Inner Niger Delta 192:Inner Niger Delta 180:Inner Niger Delta 161: 160: 1755: 1625:King Fahd Bridge 1618:Dams and bridges 1412: 1359: 1352: 1345: 1336: 1335: 1329: 1328: 1326: 1324: 1298: 1289: 1288: 1286: 1284: 1269: 1254: 1253: 1251: 1249: 1234: 1223: 1222: 1220: 1218: 1199: 1190: 1189: 1187: 1185: 1171: 1165: 1164: 1162: 1160: 1153:, Vol. 4, No. 3" 1145: 1136: 1135: 1133: 1131: 1108: 1102: 1101: 1099: 1097: 1083: 1077: 1076: 1074: 1072: 1059: 1053: 1052: 1050: 1048: 1025: 1014: 1013: 1011: 1009: 986: 980: 979: 977: 975: 952: 943: 942: 940: 938: 915: 909: 908: 906: 904: 881: 875: 874: 872: 870: 847: 841: 840: 838: 836: 830: 823: 815: 806: 805: 789: 783: 782: 780: 779: 763: 754: 753: 751: 749: 734: 623:Lake Walado Débo 584:ferruginous duck 435:Vossia cuspidata 382:, vegetation of 379:Cynodon dactylon 341:The lake in the 292:crystalline rock 126: 125:Primary outflows 112: 104: 103: 101: 100: 99: 94: 90: 87: 86: 85: 82: 72: 54: 53: 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Retrieved 742:the original 711:transhumance 688: 671: 654: 646: 640: 638: 608: 580:purple heron 537: 517:Nile monitor 509:dama gazelle 486: 482:Hippopotamus 467:Algal blooms 463: 451: 433: 427: 423: 417: 410: 404: 398: 388: 377: 356: 340: 327: 319: 307:alluvial fan 289: 269: 225: 163: 162: 154:Surface area 16:Lake in Mali 1748:Niger River 1635:Markala Dam 1604:Kainji Lake 1532:Brass River 1512:Benue River 1445:Niger Delta 1440:Lower Niger 1366:Niger River 1064:West Africa 794:Imago Mundi 695:Bani Rivers 679:Markala Dam 648:Gobiocichla 568:glossy ibis 556:sand martin 391:Walado Débo 315:Erg of Bara 296:Precambrian 272:Bani Rivers 232:Niger River 228:inner delta 200:Niger River 196:inner delta 184:Niger River 176:Niger River 131:Niger River 117:Niger River 96: / 71:Coordinates 1732:Categories 1650:Kainji Dam 1640:Gao Bridge 1502:Sota River 1482:Bani River 1477:Milo River 1175:"Lac Débo" 778:2013-04-23 717:References 665:Cyprinidae 661:Mochokidae 657:Mormyridae 634:giant barb 552:Afrotropic 548:Palearctic 384:dūrvā gras 369:Vegetation 347:Tombouctou 285:Issa Baris 276:lacustrine 1700:disasters 1655:Jebba Dam 1527:Nun River 1373:Countries 689:When the 675:leuciscus 572:spoonbill 440:wild rice 299:sandstone 258:Geography 164:Lake Débo 81:15°19′0″N 58:Lake Débo 22:Lake Débo 1609:Lac Debo 1568:Timbuktu 1418:Sections 1323:10 March 1283:22 March 1248:21 March 1217:22 March 1184:21 March 1159:21 March 1130:10 March 1096:20 March 1071:20 March 1047:20 March 1008:20 March 974:20 March 937:20 March 903:20 March 869:20 March 835:22 March 748:18 March 673:Brycinus 645:and the 540:avifauna 359:Timbuktu 311:laterite 303:Syncline 240:Timbuktu 234:between 208:Timbuktu 202:between 188:Timbuktu 1588:Onitsha 1548:Siguiri 1400:Nigeria 697:are in 685:Culture 650:wonderi 459:ecology 424:bourgou 400:bourgou 337:Climate 248:barbell 244:Ptolemy 214:History 182:of the 84:4°6′0″W 1583:Lokoja 1578:Niamey 1553:Bamako 1541:Cities 1458:) and 1380:Guinea 1314:  1121:  1038:  999:  965:  928:  894:  860:  663:, and 619:Ramsar 615:UNESCO 530:Artis 493:Hippos 448:bartti 409:, and 395:acacia 331:Niamey 323:nomads 305:as an 1597:Lakes 1563:Mopti 1558:Segou 1395:Benin 1390:Niger 829:(PDF) 822:(PDF) 699:spate 691:Niger 604:gulls 544:Sahel 473:Fauna 420:Amiro 351:Mopti 343:Sahel 236:Jenne 204:Jenne 166:is a 138:Basin 1456:list 1385:Mali 1325:2013 1312:ISBN 1285:2013 1250:2013 1219:2013 1186:2013 1161:2013 1132:2013 1119:ISBN 1098:2013 1073:2013 1049:2013 1036:ISBN 1010:2013 997:ISBN 976:2013 963:ISBN 939:2013 926:ISBN 905:2013 892:ISBN 871:2013 858:ISBN 853:Mali 837:2012 750:2013 707:Fula 703:Bozo 693:and 639:The 632:The 594:and 592:ruff 558:and 550:and 538:The 519:and 487:The 446:and 281:Dire 252:Nile 238:and 206:and 172:Mali 168:lake 144:Mali 1573:Gao 798:doi 294:of 230:of 198:of 1734:: 1293:^ 1258:^ 1227:^ 1205:. 1194:^ 1177:. 1140:^ 1018:^ 947:^ 810:^ 758:^ 725:^ 681:. 659:, 613:, 606:. 590:, 586:, 582:, 578:, 574:, 570:, 566:, 562:, 523:. 511:, 507:, 503:, 1358:e 1351:t 1344:v 1327:. 1287:. 1252:. 1221:. 1188:. 1163:. 1134:. 1100:. 1075:. 1051:. 1012:. 978:. 941:. 907:. 873:. 839:. 804:. 800:: 781:. 752:. 534:. 455:, 442:(

Index


Lake Débo is located in Mali
15°19′0″N 4°6′0″W / 15.31667°N 4.10000°W / 15.31667; -4.10000
Primary inflows
Niger River
Primary outflows
Niger River
Basin
Mali
lake
Mali
Niger River
Inner Niger Delta
Niger River
Timbuktu
Inner Niger Delta
inner delta
Niger River
Jenne
Timbuktu

inner delta
Niger River
Jenne
Timbuktu
Ptolemy
barbell
Nile

Bani Rivers

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