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Lake Magadi

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magadiite in the High Magadi Beds are filled with mud, silt and sand from overlying sediments. Their stratigraphic context reveals upward-shallowing cycles from mud to interlaminated mud-magadiite to magadiite in dm-scale units. The burrows were formed when the lake floor became fresher and oxygenated, after a period when magadiite precipitated in shallow saline waters. The burrows, probably produced by beetles, show that trace fossils can provide evidence for short-term (possibly years to decades) changes in the contemporary environment that might not otherwise be recognised or preserved physically or chemically in the sediment record.
408: 348: 87: 57: 372: 360: 384: 396: 43: 94: 64: 271:), the Magadi basin held a freshwater lake with many fish, whose remains are preserved in the High Magadi Beds, a series of lacustrine and volcaniclastic sediments preserved in various locations around the present shoreline. Evidence also exists for several older Pleistocene precursor lakes that were much larger than the present Lake Magadi. At times, Lake Magadi and 246:
in this arid region. Most hot springs lie along the northwestern and southern shorelines of the lake. During the rainy season, a thin (less than 1 m) layer of brine covers much of the saline pan, but this evaporates rapidly leaving a vast expanse of white salt that cracks to produce large polygons. A
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sp.), and birds including flamingos. Burrows discovered in outcrops of the High Magadi Beds (~25–9 ka) that predate the modern saline (trona) pan show that beetles and other invertebrates inhabit this extreme environment when conditions become more favourable. Burrows (cm-scale) preserved in
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Magadiite, a rare hydrous sodium-silicate mineral , was discovered about 50 years ago in sediments around Lake Magadi, a hypersaline alkaline lake fed by hot springs in the semi-arid southern Kenya Rift Valley. Today this harsh lacustrine environment excludes most organisms except microbial
282:. There are many varieties including bedded cherts that formed in the lake and intrusive dike-like bodies that penetrated through overlying sediments while the silica was soft. The most famous is the "Magadi-type chert", which formed from a sodium silicate mineral precursor 256:, inhabits the hot, highly alkaline waters of this lake basin and is commonly seen in some of the hot spring pools around the shoreline, where the water temperature is less than 45 °C. 518:
Eugster, H.P. 1980. Lake Magadi, Kenya, and its Pleistocene precursors. In Nissenbaum, A. (Editor) Hypersaline brines and evaporitic environments. Elsevier, Amsterdam, pp. 195–232.
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that crosses the lake provides access to the area west of the lake (Nguruman Escarpment). Recently accommodation for tourists is provided in air conditioned canvas tents.
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Behr, H.J. 2002. Magadiite and Magadi chert: a critical analysis of the silica sediments in the Lake Magadi Basin, Kenya. SEPM Special Publication 73, p. 257-273.
454:"Animal bioturbation preserved in Pleistocene magadiite at Lake Magadi, Kenya Rift Valley, and its implications for the depositional environment of bedded magadiite" 521:
Jones, B.F., Eugster, H.P., and Rettig, S.L. 1977. Hydrochemistry of the Lake Magadi basin, Kenya. Geochimica et Cosmochimica Acta, v. 41, p. 53-72.
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Eugster, H.P. 1970. Chemistry and origin of the brines from Lake Magadi, Kenya. Mineralogical Society of America Special Paper, No. 3, p. 215-235.
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Buatois, Luis A.; Renaut, Robin W.; Owen, Richard Bernhart; Behrensmeyer, Anna K.; Scott, Jennifer J. (2020-04-22).
242:(temperatures up to 86 °C) that discharge into alkaline "lagoons" around the lake margins, there being little 962: 952: 942: 982: 977: 555: 425: 318: 238:(sodium sesquicarbonate). In places, the salt is up to 40 m thick. The lake is recharged mainly by saline 972: 967: 947: 957: 926: 699: 17: 509:
Baker, B.H. 1958. Geology of the Magadi area. Report of the Geological Survey of Kenya, 42, 81 pp.
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Not to be confused with the lake in Tanzania's Ngorongoro crater which is also called
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Lake Magadi was not always so saline. Several thousand years ago (during the late
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extremophiles, a few invertebrates (mostly insects), highly adapted fish (
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Lake Magadi is also well known for its extensive deposits of siliceous
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Not to be confused with the former lake (paleolake) in Botswana called
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in the north of Kenya, where the book and film are set.
316:The lake is featured in Fernando Meirelles's film 1107: 126: 234:, precipitates vast quantities of the mineral 200:. During the dry season, it is 80% covered by 684: 556: 698: 286:that was discovered at Lake Magadi in 1967. 309:since December 2005. This factory produces 691: 677: 563: 549: 487: 469: 424:Lake Magadi another alkaline lake in the 313:, which has a range of industrial uses. 1048:Paleontological and archeological sites 1108: 1126:Saline lakes of the Great Rift Valley 672: 544: 275:were united as a single larger lake. 93: 63: 13: 570: 14: 1137: 525: 406: 394: 382: 370: 358: 353:Lake Magadi, as seen from space. 346: 330:, and is used as a stand-in for 192:is the southernmost lake in the 183:100 km (39 sq mi) 92: 85: 62: 55: 41: 445: 413:Salt harvesting at lake Magadi 1: 963:Mount Kipipiri Forest Reserve 953:Lake Bogoria National Reserve 943:Kerio Valley National Reserve 438: 983:Mount Longonot National Park 426:Ngorongoro Conservation Area 7: 973:Lake Naivasha National Park 532:Slide show of aerial photos 418: 10: 1142: 968:Kigio Wildlife Conservancy 948:Lake Baringo National Park 471:10.1038/s41598-020-63505-7 247:single species of fish, a 204:and is well known for its 30:Lake Kajiado County, Kenya 22: 15: 1121:Endorheic lakes of Africa 1047: 1001: 978:Hell's Gate National Park 958:Lake Nakuru National Park 935: 874: 818: 772: 706: 578: 534:by Christophe Gruault at 215:Lake Magadi is a saline, 179: 175: 164: 125: 115: 49: 40: 35: 700:Great Rift Valley, Kenya 322:, which is based on the 988:Mount Suswa Conservancy 927:Southern Ewaso Ng'iro 773:Hills and escarpments 428:in Northern Tanzania. 324:book of the same name 319:The Constant Gardener 301:township lies on the 993:Shompole Conservancy 269:African humid period 790:Nguruman Escarpment 145: /  936:Conservation areas 795:Losiolo Escarpment 458:Scientific Reports 194:Kenyan Rift Valley 120:Kenyan Rift Valley 106:Show map of Africa 1103: 1102: 780:Elgeyo Escarpment 666: 665: 432:Lake Makgadikgadi 253:Alcolapia grahami 187: 186: 76:Show map of Kenya 25:Lake Makgadikgadi 1133: 693: 686: 679: 670: 669: 565: 558: 551: 542: 541: 502: 501: 491: 473: 449: 410: 398: 386: 374: 362: 350: 229:sodium carbonate 160: 159: 157: 156: 155: 150: 149:1.917°S 36.267°E 146: 143: 142: 141: 138: 128: 107: 96: 95: 89: 77: 66: 65: 59: 45: 33: 32: 1141: 1140: 1136: 1135: 1134: 1132: 1131: 1130: 1106: 1105: 1104: 1099: 1043: 997: 931: 870: 814: 768: 714:Barrier Volcano 702: 697: 667: 662: 574: 569: 528: 506: 505: 450: 446: 441: 421: 414: 411: 402: 399: 390: 387: 378: 375: 366: 363: 354: 351: 221:endorheic basin 168: countries 153: 151: 147: 144: 139: 136: 134: 132: 131: 111: 110: 109: 108: 105: 104: 103: 102: 101: 97: 80: 79: 78: 75: 74: 73: 72: 71: 67: 31: 28: 21: 12: 11: 5: 1139: 1129: 1128: 1123: 1118: 1116:Lakes of Kenya 1101: 1100: 1098: 1097: 1095:Rusinga Island 1092: 1087: 1082: 1077: 1072: 1067: 1062: 1057: 1051: 1049: 1045: 1044: 1042: 1041: 1036: 1031: 1026: 1021: 1016: 1011: 1005: 1003: 999: 998: 996: 995: 990: 985: 980: 975: 970: 965: 960: 955: 950: 945: 939: 937: 933: 932: 930: 929: 924: 919: 914: 909: 904: 899: 894: 889: 884: 878: 876: 872: 871: 869: 868: 863: 858: 853: 848: 843: 838: 833: 828: 822: 820: 816: 815: 813: 812: 807: 802: 800:Aberdare Range 797: 792: 787: 785:Mau Escarpment 782: 776: 774: 770: 769: 767: 766: 761: 756: 751: 746: 741: 736: 731: 726: 724:Emuruangogolak 721: 716: 710: 708: 704: 703: 696: 695: 688: 681: 673: 664: 663: 661: 660: 655: 650: 645: 640: 635: 630: 625: 620: 615: 610: 605: 600: 595: 590: 585: 579: 576: 575: 572:Lakes of Kenya 568: 567: 560: 553: 545: 539: 538: 527: 526:External links 524: 523: 522: 519: 516: 513: 510: 504: 503: 443: 442: 440: 437: 436: 435: 429: 420: 417: 416: 415: 412: 405: 403: 400: 393: 391: 388: 381: 379: 376: 369: 367: 364: 357: 355: 352: 345: 244:surface runoff 185: 184: 181: 177: 176: 173: 172: 169: 162: 161: 154:-1.917; 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Index

Lake Magadi
Lake Makgadikgadi

Location of Lake Magadi in Kenya.
Location of Lake Magadi in Kenya.
Kenyan Rift Valley
1°55′S 36°16′E / 1.917°S 36.267°E / -1.917; 36.267
Basin
Kenyan Rift Valley
Lake Natron
soda
wading birds
flamingos
alkaline lake
endorheic basin
graben
sodium carbonate
brine
trona
hot springs
surface runoff
cichlid
Alcolapia grahami
Pleistocene
Holocene
African humid period
Lake Natron
chert
magadiite
Magadi

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