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Geology of Lesotho

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and alluvial gravel. The country has the highest concentration of kimberlite bodies in the world—a total of more than 400, including 343 dikes, 39 pipes and 23 blows. Northern Lesotho has an average of one kimberlite body for every 10 square kilometers. In spite of the large deposits, very few sites
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between the Molteno and the overlying 70 to 250 meter thick sandstones, mudstones and siltstones of the Elliot Formation, which contains silicified wood and dinosaur fossils. The 15 to 250 meter thick Clarens Formation lies atop the Elliot Formation and has sandstones, siltstones and thin bands of
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are mined and research is ongoing into alluvial deposits. The Karoo Supergroup hosts low-grade uranium and likely coal and coal-bed methane, although the Lower Karoo which hosts the coal seams does not outcrop in Lesotho. The country has quarrying of
153:. As a result, extreme erosion formed cobble beds with sand and clay layers in lower elevation valleys, with material up to 20 meters thick. Donga is a local term for the steep-sided ravines common in Lesotho that formed in this material. 193:. Dolerite-dike related aquifers have high water productivity in fractures that formed in the surrounding rock due to the high temperature of the intrusion. The sandstones of the 138:. The numerous layers of ropy plateau basalt are intruded by 70 volcanic vents and over 1000 dikes and sills. Kimberlite pipes may have formed during eruptions in the 52:
crystalline basement rock that formed 3.6 to 2.5 billion years ago. Geologists have gleaned insights into Lesotho's deep past through extrapolation from South Africa,
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is regarded as the best aquifer in Lesotho with high yield and frequent springs. Steep terrain, rain and snow melt mean that Lesotho has a high risk of landslides.
28:. The country is notable for large fossil deposits and intense erosion due to high rainfall and a rare case of southern African glaciation during the last ice age. 572: 412: 169:
and the sediments of the Karoo Supergroup were influenced by deformation at three different times before, during and after the formation of the
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More than 50% of Lesotho's territory is underlain by fractured igneous rock aquifers, such as the low permeability basalt of the
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is the only large fault in the country, running northeast–southwest with a vertical displacement of 300 meters near
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and the oldest Karoo-related unit in Lesotho, with red and maroon sandstones interspersed with thin coal seams. The
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and other data from drilling. Above the ancient basement rocks, almost all of the rocks in Lesotho are part of the
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Lesotho experienced high rainfall and was one of the few places in southern Africa glaciated during the
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The Karoo Supergroup began to form 510 million years ago in a rift valley in the south of the
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is built on ancient crystalline basement rock up to 3.6 billion years old, belonging to the
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has extensive diamonds and other natural resources and has the highest concentration of
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fine-grained basalts and sandstones in the Elliot, Molteno and Clarens Formations.
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lake bed environment, with abundant plant and insect fossils. There is an
178: 162: 146: 119: 71: 29: 131: 327: 108: 98:. The Molteno Formation is 15 to 300 meters thick and records a 331: 64:, the most widespread stratigraphic unit in southern Africa. 300: 298: 74:, spanning into what is now southern South America. The 671: 646: 365: 217:Lesotho has extensive diamond deposits in both 343: 8: 205:are small or low quality aquifers, but the 181:, although there are other smaller faults. 44:Lesotho shares many commonalities with the 350: 336: 328: 304: 289: 277: 255: 142:marking an end to volcanic activity. 7: 165:within the larger southern African 40:Stratigraphy & Geologic History 14: 658:Sahrawi Arab Democratic Republic 428:Democratic Republic of the Congo 240: 157:Structural geology and tectonics 122:enriched volcanic rocks of the 1: 267:. Springer. pp. 140–142. 36:pipes anywhere in the world. 320:. British Geological Survey. 773: 265:Geological Atlas of Africa 318:"Hydrogeology of Lesotho" 263:SchlĂĽter, Thomas (2008). 413:Central African Republic 213:Natural resource geology 136:tholeiitic magma series 86:is divided between the 78:is the top unit of the 46:geology of South Africa 573:SĂŁo TomĂ© and PrĂ­ncipe 433:Republic of the Congo 203:Burgersdorp Formation 76:Burgersdorp Formation 648:States with limited 292:, pp. 140–142. 134:that cooled from a 757:Geology of Lesotho 359:Geology of Africa 18:geology of Lesotho 744: 743: 675:other territories 448:Equatorial Guinea 228:Drakensberg Group 207:Molteno Formation 195:Clarens Formation 191:Lesotho Formation 128:Drakensberg Group 124:Lesotho Formation 96:Clarens Formation 88:Molteno Formation 764: 736: 735:(United Kingdom) 731:Tristan da Cunha 727:Ascension Island 719: 706: 697: 673:Dependencies and 366:Sovereign states 352: 345: 338: 329: 322: 321: 314: 308: 302: 293: 287: 281: 275: 269: 268: 260: 250: 245: 244: 199:Elliot Formation 175:Hellspoort fault 161:Lesotho forms a 92:Elliot Formation 62:Karoo Supergroup 58:kimberlite pipes 26:Karoo Supergroup 772: 771: 767: 766: 765: 763: 762: 761: 747: 746: 745: 740: 739: 734: 717: 704: 695: 676: 674: 667: 651: 649: 642: 361: 356: 326: 325: 316: 315: 311: 303: 296: 288: 284: 276: 272: 262: 261: 257: 246: 239: 236: 226:clay deposits, 215: 187: 173:mountains. The 159: 84:Stormberg Group 56:extracted from 50:Kaapvaal Craton 42: 22:Kaapvaal Craton 12: 11: 5: 770: 768: 760: 759: 749: 748: 742: 741: 738: 737: 720: 707: 698: 684:Canary Islands 680: 679: 677: 672: 669: 668: 666: 665: 660: 654: 652: 647: 644: 643: 641: 640: 635: 630: 625: 620: 615: 610: 605: 600: 595: 590: 585: 580: 575: 570: 565: 560: 555: 550: 545: 540: 535: 530: 525: 520: 515: 510: 505: 500: 495: 490: 485: 480: 475: 470: 465: 460: 455: 450: 445: 440: 435: 430: 425: 420: 415: 410: 405: 400: 395: 390: 385: 380: 375: 369: 367: 363: 362: 357: 355: 354: 347: 340: 332: 324: 323: 309: 307:, p. 142. 294: 282: 280:, p. 140. 270: 254: 253: 252: 251: 248:Geology portal 235: 232: 214: 211: 186: 183: 158: 155: 116:Early Jurassic 80:Beaufort Group 69:supercontinent 41: 38: 13: 10: 9: 6: 4: 3: 2: 769: 758: 755: 754: 752: 732: 728: 724: 721: 715: 711: 708: 702: 699: 693: 689: 685: 682: 681: 678: 670: 664: 661: 659: 656: 655: 653: 645: 639: 636: 634: 631: 629: 626: 624: 621: 619: 616: 614: 611: 609: 606: 604: 601: 599: 596: 594: 591: 589: 586: 584: 581: 579: 576: 574: 571: 569: 566: 564: 561: 559: 556: 554: 551: 549: 546: 544: 541: 539: 536: 534: 531: 529: 526: 524: 521: 519: 516: 514: 511: 509: 506: 504: 501: 499: 496: 494: 491: 489: 488:Guinea-Bissau 486: 484: 481: 479: 476: 474: 471: 469: 466: 464: 461: 459: 456: 454: 451: 449: 446: 444: 441: 439: 436: 434: 431: 429: 426: 424: 421: 419: 416: 414: 411: 409: 406: 404: 401: 399: 396: 394: 391: 389: 386: 384: 381: 379: 376: 374: 371: 370: 368: 364: 360: 353: 348: 346: 341: 339: 334: 333: 330: 319: 313: 310: 306: 305:SchlĂĽter 2008 301: 299: 295: 291: 290:SchlĂĽter 2008 286: 283: 279: 278:SchlĂĽter 2008 274: 271: 266: 259: 256: 249: 243: 238: 233: 231: 229: 225: 220: 212: 210: 208: 204: 200: 196: 192: 184: 182: 180: 176: 172: 168: 164: 156: 154: 152: 148: 143: 141: 137: 133: 129: 126:(part of the 125: 121: 117: 112: 110: 105: 101: 100:Late Triassic 97: 93: 89: 85: 81: 77: 73: 70: 65: 63: 59: 55: 51: 47: 39: 37: 35: 31: 27: 23: 19: 723:Saint Helena 694:   598:South Africa 588:Sierra Leone 502: 393:Burkina Faso 312: 285: 273: 264: 258: 216: 188: 185:Hydrogeology 160: 144: 113: 104:unconformity 66: 43: 17: 15: 650:recognition 603:South Sudan 493:Ivory Coast 219:kimberlites 171:Drakensberg 167:Karoo Basin 151:Pleistocene 705:(Portugal) 663:Somaliland 583:Seychelles 548:Mozambique 533:Mauritania 518:Madagascar 473:The Gambia 408:Cape Verde 234:References 224:Quaternary 140:Cretaceous 34:kimberlite 538:Mauritius 54:xenoliths 751:Category 729: / 725: / 718:(France) 712: / 690: / 686: / 638:Zimbabwe 613:Tanzania 463:Ethiopia 458:Eswatini 438:Djibouti 403:Cameroon 388:Botswana 179:Mafeteng 163:syncline 147:Cenozoic 120:amygdale 72:Gondwana 714:RĂ©union 710:Mayotte 701:Madeira 696:(Spain) 692:Melilla 623:Tunisia 593:Somalia 578:Senegal 563:Nigeria 553:Namibia 543:Morocco 508:Liberia 503:Lesotho 453:Eritrea 423:Comoros 398:Burundi 373:Algeria 145:In the 48:, with 30:Lesotho 733:  716:  703:  633:Zambia 628:Uganda 568:Rwanda 523:Malawi 483:Guinea 378:Angola 132:basalt 688:Ceuta 608:Sudan 558:Niger 513:Libya 498:Kenya 478:Ghana 468:Gabon 443:Egypt 383:Benin 109:chert 618:Togo 528:Mali 418:Chad 201:and 114:The 94:and 16:The 753:: 297:^ 197:, 118:, 111:. 90:, 351:e 344:t 337:v

Index

Kaapvaal Craton
Karoo Supergroup
Lesotho
kimberlite
geology of South Africa
Kaapvaal Craton
xenoliths
kimberlite pipes
Karoo Supergroup
supercontinent
Gondwana
Burgersdorp Formation
Beaufort Group
Stormberg Group
Molteno Formation
Elliot Formation
Clarens Formation
Late Triassic
unconformity
chert
Early Jurassic
amygdale
Lesotho Formation
Drakensberg Group
basalt
tholeiitic magma series
Cretaceous
Cenozoic
Pleistocene
syncline

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