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Journal articles on the topic 'Geology (Lesotho)'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

MASTER, S. "Henry Edward Richard Bright: a forgotten pioneer of the geological and palaeontological exploration of Lesotho in the 1870s." Archives of Natural History 35, no. 2 (2008): 191–202. http://dx.doi.org/10.3366/e0260954108000338.

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All existing accounts of the geology of Lesotho (formerly Basutoland), in southern Africa, refer to the pioneering efforts of the Revd S. S. Dornan, published between 1905 and 1908, as the first geological works in this country. However, one Henry Edward Richard Bright had already published two papers on Basutoland geology in the Cape monthly magazine, in 1873 and 1874. The first paper dealt with an uneconomic twelve-inch coal seam south of Maseru. It was accompanied by a sketch map and the first published geological cross-section through any part of Lesotho. In the second paper, dealing with

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2

Steyer, J. Sébastien, and Ross Damiani. "A giant brachyopoid temnospondyl from the Upper Triassic or Lower Jurassic of Lesotho." Bulletin de la Société Géologique de France 176, no. 3 (2005): 243–48. http://dx.doi.org/10.2113/176.3.243.

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Abstract A jaw fragment of a giant temnospondyl from the Upper Triassic or Lower Jurassic of Lesotho (southern Africa), initially regarded as a Triassic mastodonsaurid because of its size, is redescribed in detail and considered to be a member of the Brachyopoidea (Brachyopidae + Chigutisauridae sensu Warren and Marsicano [2000]) based on its dental morphology, presence of a well-developed ectopterygoid tusk, and the concavity of the ventral margin of the skull in lateral view. Recognition of the specimen as a brachyopid, rather than as a chigutisaurid, is of palaeobiogeographical significance

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3

Backeus, Ingvar. "Flarks in the Maloti, Lesotho." Geografiska Annaler. Series A, Physical Geography 71, no. 1/2 (1989): 105. http://dx.doi.org/10.2307/521014.

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4

Calles, Bengt, and Lena Kulander. "Rainfall Erosivity at Roma, Lesotho." Geografiska Annaler. Series A, Physical Geography 76, no. 1/2 (1994): 121. http://dx.doi.org/10.2307/521325.

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5

Calles, Bengt, and Lena Kulander. "Rainfall Erosivity at Roma, Lesotho." Geografiska Annaler: Series A, Physical Geography 76, no. 1-2 (1994): 121–29. http://dx.doi.org/10.1080/04353676.1994.11880411.

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6

KNOLL, F. "A primitive sauropodomorph from the upper Elliot Formation of Lesotho." Geological Magazine 147, no. 6 (2010): 814–29. http://dx.doi.org/10.1017/s001675681000018x.

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AbstractA well-preserved, articulated dinosaur skeleton from southern Africa is described. The specimen comes from the upper Elliot Formation (?Hettangian) of Ha Ralekoala (Lesotho) and represents a new species:Ignavusaurus rachelisgenus et species nova. A cladistic analysis suggests thatIgnavusaurusis more derived thanThecodontosaurus–Pantydraco, but more primitive thanEfraasia.Ignavusaurusindeed shares a number of unambiguous synapomorphies with the taxa more derived thanThecodontosaurus–Pantydraco, such as a fully open acetabulum, but it is more plesiomorphic thanEfraasiaand more derived sa

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7

de Graaf, P. J. H., and F. G. Bell. "The Delivery Tunnel North, Lesotho highlands water project." Geotechnical & Geological Engineering 15, no. 2 (1997): 95–120. http://dx.doi.org/10.1007/bf00880752.

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8

Cairncross, Bruce, and Herman du Plessis. "Stilbite and Associated Minerals from the Butha-Buthe District, Lesotho, Southern Africa." Rocks & Minerals 93, no. 4 (2018): 306–19. http://dx.doi.org/10.1080/00357529.2018.1454104.

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9

Rydgren, Bernt. "A Geomorphological Approach to Soil Erosion Studies in Lesotho." Geografiska Annaler. Series A, Physical Geography 70, no. 3 (1988): 255. http://dx.doi.org/10.2307/521078.

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10

Grab, S. W., and S. C. Mills. "Quaternary slope processes and morphologies in the upper Sehonghong Valley, eastern Lesotho." Proceedings of the Geologists' Association 122, no. 1 (2011): 179–86. http://dx.doi.org/10.1016/j.pgeola.2010.02.001.

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11

Grab, Stefan. "Rock‐surface temperatures of basalt in the drakensberg alpine environment, lesotho." Geografiska Annaler: Series A, Physical Geography 89, no. 3 (2007): 185–93. http://dx.doi.org/10.1111/j.1468-0459.2007.00317.x.

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12

Bell, F. G., P. J. H. De Graaf, and D. R. Haskins. "A geoteehnical survey of phase 1A of the Lesotho Highlands Water Project." Quarterly Journal of Engineering Geology and Hydrogeology 28, no. 4 (1995): 317–32. http://dx.doi.org/10.1144/gsl.qjegh.1995.028.p4.02.

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13

van Rooy, J. L., and A. van Schalkwyk. "The geology of the Lesotho Highlands Water Project with special reference to the durability of construction materials." Journal of African Earth Sciences (and the Middle East) 16, no. 1-2 (1993): 181–92. http://dx.doi.org/10.1016/0899-5362(93)90166-n.

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14

Nel, Werner, and Paul Sumner. "Rainfall and temperature attributes on the lesotho–drakensberg escarpment edge, southern africa." Geografiska Annaler: Series A, Physical Geography 90, no. 1 (2008): 97–108. http://dx.doi.org/10.1111/j.1468-0459.2008.00337.x.

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15

Sumner, P. D. "Geomorphic and climatic implications of relict openwork block accumulations near thabana‐ntlenyana, lesotho." Geografiska Annaler: Series A, Physical Geography 86, no. 3 (2004): 289–302. http://dx.doi.org/10.1111/j.0435-3676.2004.00232.x.

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16

Knoll, Fabien. "The tetrapod fauna of the Upper Elliot and Clarens formations in the main Karoo Basin (South Africa and Lesotho)." Bulletin de la Société Géologique de France 176, no. 1 (2005): 81–91. http://dx.doi.org/10.2113/176.1.81.

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Abstract In the main Karoo Basin (southern Africa), the “Stormberg Group” can be divided into at least two faunal zones on the basis of its palaeontological content. The upper one encompasses the Upper Elliot and Clarens formations (“Upper Stormberg Group”). It is well known for its prosauropod and cynodont fauna, but it has also yielded some ste-reospondyl remains, a turtle, at least one lepidosaur, a small variety of crocodylomorphs, rare theropod elements, and an assortment of ornithischians. The presence of pterosaurs is put forward on ichnological grounds, but aetosaur and rauisuchian rep

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17

Castro, D. J., and F. G. Bell. "An engineering geological appraisal of the sandstones of the Clarens Formation, Lesotho, in relation to tunnelling." Geotechnical and Geological Engineering 13, no. 3 (1995): 117–42. http://dx.doi.org/10.1007/bf00456713.

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18

Muavhi, Nndanduleni, and Abera Tessema. "Identification of potential targets for kimberlite exploration using satellite imagery and map combination approach in the Lesotho Kimberlite Province." Ore Geology Reviews 132 (May 2021): 104001. http://dx.doi.org/10.1016/j.oregeorev.2021.104001.

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19

de Wit, M. J., B. Linol, H. Furnes, T. Muedi, and K. Valashiya. "Pillow Talk: Volcanic rocks of the Karoo that formed many leagues under the Gondwanan Sea." South African Journal of Geology 123, no. 3 (2020): 297–330. http://dx.doi.org/10.25131/sajg.123.0021.

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Abstract New field mapping has discovered numerous sections of pillow lavas with hyaloclastites at the lowest levels of Jurassic Karoo volcanic sequences across Lesotho and South Africa. Vesicularity (content and size) and geochemistry of the ca. 1 to 50 m thick pillow lavas sequences presently preserved at 1 670 to 2 150 m asl reveal they originated below 500 m of water. Most of the initial 87Sr/86Sr ratios of the pillow lavas scatter around ca. 0.708, which is also the value of Jurassic seawater. There is an increase in the δ18O values concomitantly with increasing alteration, a well-known f

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20

Boniface, A., J. G. McKelvey, and S. Nthako. "Planning and design of the transfer tunnel for the Lesotho highlands water project." Tunnelling and Underground Space Technology 9, no. 1 (1994): 79–89. http://dx.doi.org/10.1016/0886-7798(94)90013-2.

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21

Galloway, M., T. Nowicki, B. van Coller, et al. "Constraining kimberlite geology through integration of geophysical, geological and geochemical methods: A case study of the Mothae kimberlite, northern Lesotho." Lithos 112 (November 2009): 130–41. http://dx.doi.org/10.1016/j.lithos.2009.06.026.

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22

Davies, A. G. "An introductory description of the Lesotho highlands water project, emphasizing implementation of phase IA." Tunnelling and Underground Space Technology 9, no. 1 (1994): 73–78. http://dx.doi.org/10.1016/0886-7798(94)90012-4.

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23

Grab, Stefan. "Block and debris deposits in the high drakensberg, lesotho, southern africa: implications for high altitude slope processes." Geografiska Annaler: Series A, Physical Geography 81, no. 1 (1999): 1–16. http://dx.doi.org/10.1111/j.0435-3676.1999.00045.x.

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24

Parker, Adrian G., Julia Lee-Thorp, and Peter J. Mitchell. "Late Holocene Neoglacial conditions from the Lesotho highlands, southern Africa: phytolith and stable carbon isotope evidence from the archaeological site of Likoaeng." Proceedings of the Geologists' Association 122, no. 1 (2011): 201–11. http://dx.doi.org/10.1016/j.pgeola.2010.09.005.

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25

Moore, A. E. "The origin of mantle-derived megacrysts and sheared peridotites-evidence from kimberlites in the northern Lesotho - Orange Free State (South Africa) and Botswana pipe clusters." South African Journal of Geology 104, no. 1 (2001): 23–38. http://dx.doi.org/10.2113/104.1.23.

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26

Tolchard, Frederick, Sterling J. Nesbitt, Julia B. Desojo, Pia Viglietti, Richard J. Butler, and Jonah N. Choiniere. "‘Rauisuchian’ material from the lower Elliot Formation of South Africa and Lesotho: Implications for Late Triassic biogeography and biostratigraphy." Journal of African Earth Sciences 160 (December 2019): 103610. http://dx.doi.org/10.1016/j.jafrearsci.2019.103610.

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27

Mills, Stephanie C., Stefan W. Grab, and Simon J. Carr. "Late quaternary moraines along the sekhokong range, eastern lesotho: contrasting the geomorphic history of north‐ and south‐facing slopes." Geografiska Annaler: Series A, Physical Geography 91, no. 2 (2009): 121–40. http://dx.doi.org/10.1111/j.1468-0459.2009.00359.x.

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28

Richards, J. A., F. Remmer, and J. C. Sharp. "Design and construction of a segmental lining for a machine-bored tunnel: Delivery tunnel North, Lesotho highlands water project." Tunnelling and Underground Space Technology 9, no. 1 (1994): 91–99. http://dx.doi.org/10.1016/0886-7798(94)90014-0.

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29

Rampersadh, Akhil, Emese M. Bordy, Lara Sciscio, and Miengah Abrahams. "Dinosaur behaviour in an Early Jurassic palaeoecosystem – uppermost Elliot Formation, Ha Nohana, Lesotho." Annales Societatis Geologorum Poloniae, 2018. http://dx.doi.org/10.14241/asgp.2018.010.

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30

"Experiences with the precast segmental lining for the Mohale Tunnel in Lesotho." Tunnelling and Underground Space Technology 19, no. 4-5 (2004): 427. http://dx.doi.org/10.1016/j.tust.2004.02.043.

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31

Knight, J., and S. W. Grab. "Stratigraphy of late Quaternary mountain slope landforms and deposits in southern Africa and their significance for the dynamics of mountain sediment systems." South African Journal of Geology, July 28, 2021. http://dx.doi.org/10.25131/sajg.124.0037.

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Abstract Mountains are areas of high potential sediment yield due to their steep slopes and generally cool, wet climates. Mountain sediments are moved by gravity-driven and often cryogenically-influenced processes, and captured within valleys or footslopes in the form of screes, alluvial/colluvial fans and terraces, or on hillslopes in the form of solifluction sheets, debris lobes/ridges and openwork block deposits. This study critically examines the geomorphic, sedimentary, stratigraphic and dating evidence from cryogenically-influenced late Quaternary slope deposits found along the highest s

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32

Scheiber-Enslin, S. E., M. Manzi, and S. J. Webb. "Seismic imaging of dolerite sills and volcanic vents in the Central Karoo, South Africa: implications for shale gas potential." South African Journal of Geology, July 9, 2021. http://dx.doi.org/10.25131/sajg.124.0043.

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Abstract The Karoo Basin of South Africa covers an area of 700 000 km2 and has been identified as a possible shale gas reserve. Any evaluation of the shale gas potential of the basin must consider the widespread dolerite dykes and sills. These intrusions were emplaced into the Karoo Supergroup and are well dated at around 183 Ma. Their intrusion triggered the explosive releases of gas in the basin, marked on surface by breccia pipes and hydrothermal vents. This outpouring of gas has been proposed as a significant contributor to global climate change. Research into the three-dimensional interco

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