DOCSLIB.ORG

I T-H G, Eaggy Gem-R

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
I T-H G, Eaggy Gem-R ese * I t-h eaggy Gem-r g g, CII.Cr~rd'Sc .htz Lesotho T,,/ Geology, Geomorphology, Soils G. Schmitz F. Rooyani National University of Lesotho 1987 The Authors: Gerard Schmitz, Ph.D. Professor of Geography. Applied Environmental Sciences Programme Department of Geography. National University of Lesotho Firouz Rooyani. Ph.D. Team Leader, Education Component of Lesotho Agricultural Production and Institutional Support Project Adjunct Assistant Professor, Department of Soil and Water Science, University of Arizona Honorary Lecturer. National University of Lesotho © 1987 G. Schmitz Funded by: The Netherlands University Foundation for International Cooperation The United States Agency for International Development The National University of Lesotho Distributed by: The National University of Lesotho Printed by Morija Printing Works - Lesotho Cover picture by Dirk Schwager Acknowledgements We wish to thank all those who gave permission for us to reproduce copyright material in this book. Information regarding sources is given in the captions. We greatly appreciate the assistance given to us in the preparation of this book by the fol­ lowing persons: Martinus Vranken, Utrecht University, for making the drawings for Sections One, Two and Three. Tom Lynn, National University of Lesotho, for editing the text. Mrs. C. Russell, USAID Mission in Lesotho, for typing the manuscript, Dr. C. Mabbs - Zeno, for taking and developing photographs of rock samples, Dr. B. Badamchian, Ministry of Agriculture and Marketing, for her comments on Section Four of this text. Preface This publication has been written for all those interested in the characteristics and dynamics of Lesotho's natural environment, especially for teachers, fieldworkers, and for students at the National University of Lesotho and at the Lesotho Agricultural College. A glossary has been added to facilitate the reading of the text, as well as a summary of the U.S. soil classification system, as the Lesotho Government has adopted it for the classification of its soils. The reader will discover that relatively little is known about the geomorphology of Lesotho, as not much research into this topic has so far been undertaken in the country. More is known about the geology of Lesotho. In 1947, G.M. Stockley published the first comprehensive study on "the geology of Basutoland". Since then, the Government's Department of Mines and Geology has undertaken to map the country and has published a good number of geological reports and maps of different scales. Much information has been obtained from studies of areas with a similar geology in the immediate surroundings of Lesotho. Soil analysis, soil mapping and soil classification have been undertaken quite exten­ sively in Lesotho, and a comprehensive general picture of the soils of Lesotho isarising. As agriculture is amajor economic activity in Lesotho, and as soils are being eroded in a drastic way, a chapter on recent processes and forms of accelerated erosion and de­ position has been included. The authors have undertaken an extensive literature survey, and to a large extent this publication is based on studies undertaken by other researchers. We hope to have given due acknowledgement to the many authors quoted, and apologise if some references have been erroneously omitted. We invite comments and criticisms of this publication, so that we may improve on our understanding of the natural environment of Lesotho. G. Schmitz Roma F. Rooyani Maseru 1987 Contents SECTION ONE: GEOLOGICAL EVOLUTION Chapter One The GeneralFramework ........................................... 3 1.1 Cratonisation .................................... 3 1.2 Gondwanaland.................................. 4 1.3 The Karoo Basin and Basin Floor Characteristics .......... 6 1.4 I..ieBoundary between the Kaapvaal Craton and the Namaqualand-Natal Circum-Cratonic Belt ................... 10 ChapterTwo Basin Sedimentation ............................... 12 2.1 Karoo Sedimentary History and Basin Floor Characteristics 12 2.2 D wyka Form ation ................................................... 12 2.3 Ecca Group .......................................................... 14 2.4 Beaufort G roup .......,W ........................................... 16 2.5 Storm berg G roup ................................................... 20 ChapterThree Magmaticand Tectonic Episodes ................................ 35 3.1 The Karoo Volcanic Episode .................................... 35 3.2 Intrusions aiid Structural Deformations ....................... 42 3.3 Kimberlite :Emplacements ........................................ 45 3.4 Seismicity ............................................................. 48 SECTION TWO: GEOLOGICAL RESOURCES ChapterFour GroundwaterResources ............................................ 59 4.1 Groundwater Occurrences ........................................ 59 4.2 Springs ................................................................. 61 4.3 Groundwater Estimates .......................................... 63 ChapterFive Mineral Resources .................................................. 64 5.1 Diamonds ............................................................. 64 5.2 Uranium ............................................................... 64 5.3 Mercury ............................................................... 66 5.4 Building Stones ...................................................... 66 5.5 Clay Deposits ....................................................... 66 SECTION THREE: GEOMORPHOLOGY Chapter Six Geomorphological Units ........................................... 69 6.1 Definition and Description ..................................... 69 6.2 Geomorphological Units and Associated Soils .............. 76 6.3 Geomorphology and Land Suitability Classification .......78 Chapter Seven Geomorphological Evolution ..................................... 85 7.1 The Formation of Planation Surfaces ......................... 85 7.2 Reorientation from Interior to Coastal Drainage ........... 91 7.3 Nivation/Glaciation Hollows ..................................... 95 Chapter Eight Accelerated Erosion and Sedimentation ........................ 98 8.1 Introduction ......................................................... 98 8.2 Erosion Processes and Forms .................................... 98 S.3 Sediment Transport and Deposition ........................... 103 8.4 Climatic Factors ..................................................... 104 8.5 Soil Factors ........................................................... 106 8.6 Terrain Factors ...................................................... 108 8.7 Human Factors ...................................................... 108 8.8 Estimation of Soil Loss and the Universal Soil Loss Equation .................................................. 111 SECTION FOUR: SOILS Chapter Nine Soil Materials ......................................................... 123 9.1 Organic Component ................................................ 123 9.2 Mineral Component ................................................ 126 Chapter Ten Soil Formation ....................................................... 130 10.1 Weathering and Formation of New Material ................. 130 10.2 Erosion and Deposition Processes .............................. 132 10.3 Eluviation and Illuviation ......................................... 134 Chapter Eleven Soil Forming Factors ............................................... 138 11.1 Climate ..... ................ ..................... 138 11.2 Vegetation ............................................................ 140 11.3 Parent Material ...................................................... 141 11.4 Topography ........................................................... 142 11.5 Genesis and Classification ......................................... 144 -A, t ChapterTwelve ImportantSoil Groupsof Lesotho: I. Mollisols ............. 147 12.1 Mollisols with an Aquic Moisture Regime .................... 148 12.2 Mollisols with a Cryic Temperature Regime ................. 150 12.3 Mollisols with a Ustic Moisture Regime ....................... 150 12.4 Mollisols with a Udic Moisture Regime ....................... 153 ChapterThirteen ImportantSoil Groups of Lesotho: I1. Alfisols .............. 157 13.1 Alfisols with an Aquic Moisture Regime ...................... 159 13.2 Alfisols with a Udic Moisture Regime Bordering on Aquic 160 13.3 Alfisols with a Udic Moisture Regime ............................ 162 13.4 Alfisols with a Ustic Moisture Regime ......................... 163 ChapterFourteen ImportantSoil GroupsofLesotho: III. Entisols, Inceptisols, Vertisols ................................................ 166 14.1 Entisols ................................................................ 166 14.2 Inceptisols ............................................................. 169 14.3 Vertisols ............................................................... 172 APPENDIX ............................................................................. 175 GLOSSARY ............................................................................. 183 REFERENCES ............................................................................. 192 IN D EX ............................................................................. 202 Section One Geological Evolution Lesotho: Geology, Geomorphology, Soils 3 Chapter One The General Framework 1.1 Cratonisation The structural development of the African continent has been marked by several
Load more

Recommended publications
  • Martian Crater Morphology
    ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter.
    [Show full text]
  • Lesotho Vulnerability Assessment Committee
    2016 Lesotho Government Lesotho VAC Table of Contents List of Tables ................................LESOTHO................................................................ VULNERABILITY.............................................................................. 0 List of Maps ................................................................................................................................................................................ 0 Acknowledgments ................................ASSESSMENT................................................................ COMMITTEE................................................................ ... 3 Key Findings .............................................................................................................................................................................. 4 Executive Summary ................................................................................................................................................................ 5 INTERVENTION MODALITY SELECTION Section 1: Objectives, methodology and limitations ................................................................................................. 7 1.1 Objectives ................................In light ................................of the findings................................ from the LVAC................................ Market Assessment................................ that assessed....... 9 the functionality and performance of Lesotho’s food markets, LVAC proceeded to 1.2 Methodology
    [Show full text]
  • 11 Fall Unamagazine
    FALL 2011 • VOLUME 19 • No. 3 FOR ALUMNI AND FRIENDS OF THE UNIVERSITY OF NORTH ALABAMA Cover Story 10 ..... Thanks a Million, Harvey Robbins Features 3 ..... The Transition 14 ..... From Zero to Infinity 16 ..... Something Special 20 ..... The Sounds of the Pride 28 ..... Southern Laughs 30 ..... Academic Affairs Awards 33 ..... Excellence in Teaching Award 34 ..... China 38 ..... Words on the Breeze Departments 2 ..... President’s Message 6 ..... Around the Campus 45 ..... Class Notes 47 ..... In Memory FALL 2011 • VOLUME 19 • No. 3 for alumni and friends of the University of North Alabama president’s message ADMINISTRATION William G. Cale, Jr. President William G. Cale, Jr. The annual everyone to attend one of these. You may Vice President for Academic Affairs/Provost Handy festival contact Dr. Alan Medders (Vice President John Thornell is drawing large for Advancement, [email protected]) Vice President for Business and Financial Affairs crowds to the many or Mr. Mark Linder (Director of Athletics, Steve Smith venues where music [email protected]) for information or to Vice President for Student Affairs is being played. At arrange a meeting for your group. David Shields this time of year Sometimes we measure success by Vice President for University Advancement William G. Cale, Jr. it is impossible the things we can see, like a new building. Alan Medders to go anywhere More often, though, success happens one Vice Provost for International Affairs in town and not hear music. The festival student at a time as we provide more and Chunsheng Zhang is also a reminder that we are less than better educational opportunities.
    [Show full text]
  • Widespread Crater-Related Pitted Materials on Mars: Further Evidence for the Role of Target Volatiles During the Impact Process ⇑ Livio L
    Icarus 220 (2012) 348–368 Contents lists available at SciVerse ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Widespread crater-related pitted materials on Mars: Further evidence for the role of target volatiles during the impact process ⇑ Livio L. Tornabene a, , Gordon R. Osinski a, Alfred S. McEwen b, Joseph M. Boyce c, Veronica J. Bray b, Christy M. Caudill b, John A. Grant d, Christopher W. Hamilton e, Sarah Mattson b, Peter J. Mouginis-Mark c a University of Western Ontario, Centre for Planetary Science and Exploration, Earth Sciences, London, ON, Canada N6A 5B7 b University of Arizona, Lunar and Planetary Lab, Tucson, AZ 85721-0092, USA c University of Hawai’i, Hawai’i Institute of Geophysics and Planetology, Ma¯noa, HI 96822, USA d Smithsonian Institution, Center for Earth and Planetary Studies, Washington, DC 20013-7012, USA e NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA article info abstract Article history: Recently acquired high-resolution images of martian impact craters provide further evidence for the Received 28 August 2011 interaction between subsurface volatiles and the impact cratering process. A densely pitted crater-related Revised 29 April 2012 unit has been identified in images of 204 craters from the Mars Reconnaissance Orbiter. This sample of Accepted 9 May 2012 craters are nearly equally distributed between the two hemispheres, spanning from 53°Sto62°N latitude. Available online 24 May 2012 They range in diameter from 1 to 150 km, and are found at elevations between À5.5 to +5.2 km relative to the martian datum. The pits are polygonal to quasi-circular depressions that often occur in dense clus- Keywords: ters and range in size from 10 m to as large as 3 km.
    [Show full text]
  • Martian Subsurface Properties and Crater Formation Processes Inferred from Fresh Impact Crater Geometries
    Martian Subsurface Properties and Crater Formation Processes Inferred From Fresh Impact Crater Geometries The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Stewart, Sarah T., and Gregory J. Valiant. 2006. Martian subsurface properties and crater formation processes inferred from fresh impact crater geometries. Meteoritics and Planetary Sciences 41: 1509-1537. Published Version http://meteoritics.org/ Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:4727301 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Meteoritics & Planetary Science 41, Nr 10, 1509–1537 (2006) Abstract available online at http://meteoritics.org Martian subsurface properties and crater formation processes inferred from fresh impact crater geometries Sarah T. STEWART* and Gregory J. VALIANT Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, Massachusetts 02138, USA *Corresponding author. E-mail: [email protected] (Received 22 October 2005; revision accepted 30 June 2006) Abstract–The geometry of simple impact craters reflects the properties of the target materials, and the diverse range of fluidized morphologies observed in Martian ejecta blankets are controlled by the near-surface composition and the climate at the time of impact. Using the Mars Orbiter Laser Altimeter (MOLA) data set, quantitative information about the strength of the upper crust and the dynamics of Martian ejecta blankets may be derived from crater geometry measurements.
    [Show full text]
  • Lesotho 2019 Human Rights Report
    LESOTHO 2019 HUMAN RIGHTS REPORT EXECUTIVE SUMMARY Lesotho is a constitutional monarchy with a democratic parliamentary government. Under the constitution the king is head of state but does not actively participate in political activities. The prime minister is head of government and has executive authority. In 2017 former prime minister Pakalitha Mosisili of the Democratic Congress Party lost a vote of no confidence and a snap election. All major parties accepted the outcome, and Motsoahae Thomas Thabane of the All Basotho Convention Party (ABC) formed a coalition government and became prime minister. Mosisili transferred power peacefully to Thabane, and Mathibeli Mokhothu assumed leadership of the opposition. Local and international observers assessed the election as peaceful, credible, and transparent. The security forces consist of the Lesotho Defense Force (LDF), the Lesotho Mounted Police Service (LMPS), the National Security Service (NSS), and the Lesotho Correctional Service (LCS). The LMPS is responsible for internal security. The LDF maintains external security and may support police when the LMPS commissioner requests assistance. The NSS is an intelligence service that provides information on possible threats to internal and external security. The LDF and NSS report to the minister of defense; the LMPS, to the minister of police and public safety; and the LCS, to the minister of justice and correctional service. Civilian authorities generally maintained effective control over the security forces. The Southern African Development Community (SADC) Preventive Mission in Lesotho contingent of troops, deployed to foster stability as the government moved forward with SADC-recommended security-sector reforms, departed the country in November 2018. In May the government did not meet an SADC deadline for completion of constitutional and security reforms.
    [Show full text]
  • First Year of Coordinated Science Observations by Mars Express and Exomars 2016 Trace Gas Orbiter
    MANUSCRIPT PRE-PRINT Icarus Special Issue “From Mars Express to ExoMars” https://doi.org/10.1016/j.icarus.2020.113707 First year of coordinated science observations by Mars Express and ExoMars 2016 Trace Gas Orbiter A. Cardesín-Moinelo1, B. Geiger1, G. Lacombe2, B. Ristic3, M. Costa1, D. Titov4, H. Svedhem4, J. Marín-Yaseli1, D. Merritt1, P. Martin1, M.A. López-Valverde5, P. Wolkenberg6, B. Gondet7 and Mars Express and ExoMars 2016 Science Ground Segment teams 1 European Space Astronomy Centre, Madrid, Spain 2 Laboratoire Atmosphères, Milieux, Observations Spatiales, Guyancourt, France 3 Royal Belgian Institute for Space Aeronomy, Brussels, Belgium 4 European Space Research and Technology Centre, Noordwijk, The Netherlands 5 Instituto de Astrofísica de Andalucía, Granada, Spain 6 Istituto Nazionale Astrofisica, Roma, Italy 7 Institut d'Astrophysique Spatiale, Orsay, Paris, France Abstract Two spacecraft launched and operated by the European Space Agency are currently performing observations in Mars orbit. For more than 15 years Mars Express has been conducting global surveys of the surface, the atmosphere and the plasma environment of the Red Planet. The Trace Gas Orbiter, the first element of the ExoMars programme, began its science phase in 2018 focusing on investigations of the atmospheric composition with unprecedented sensitivity as well as surface and subsurface studies. The coordination of observation programmes of both spacecraft aims at cross calibration of the instruments and exploitation of new opportunities provided by the presence of two spacecraft whose science operations are performed by two closely collaborating teams at the European Space Astronomy Centre (ESAC). In this paper we describe the first combined observations executed by the Mars Express and Trace Gas Orbiter missions since the start of the TGO operational phase in April 2018 until June 2019.
    [Show full text]
  • Lesotho Housing Profile.Pdf
    HS/078/15E ISBN(Series): 978-92-1-131927-9 ISBN(Volume): 978-92-1-132686-4 UNITED NATIONS HUMAN SETTLEMENTS PROGRAMME P.O.Box 30030,Nairobi 00100,Kenya; Tel: +254-20-7626742; Fax: +254-20-7625015; [email protected] www.unhabitat.org LESOTHO HOUSING PROFILE LESOTHO HOUSING PROFILE Prepared by Graham Tipple in collaboration with the Housing Department of the Ministry of Local Government, Chieftainship and Parliamentary Affairs First published in Nairobi in October 2015 by UN-Habitat. Copyright © United Nations Human Settlements Programme 2015 Produced by the Housing Unit United Nations Human Settlements Programme (UN-Habitat) P. O. Box 30030, 00100 Nairobi GPO KENYA Tel: 254-020-7623120 (Central Office) www.unhabitat.org HS/078/15E ISBN(Series): 978-92-1-131927-9 ISBN(Volume): 978-92-1-132686-4 DISCLAIMER The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers of boundaries. Views expressed in this publication do not necessarily reflect those of the United Nations Human Settlements Programme, the United Nations, or its Member States. Excerpts may be reproduced without authorization, on condition that the source is indicated. ii ACKNOWLEDGMENTS ACKNOWLEDGMENTS Supervisor: Christophe Lalande Task Managers: Gregor Herda and Kamba Ankunda Contributors: Channe Oguzhan, Fernanda Lonardoni, Kamba Ankunda and Gregor Herda Principal Author: Graham Tipple National Profile Team Coordinator: Kabelo Lethunya Design and layout: Andrew Ondoo Financial Support: The participatory Slum Upgrading Program (PSUP), a joint initiative by the European Commission and the African, Caribbean and Pacific (ACP) Secretariat and implemented by UN-Habitat, UNDP and the Government of Lesotho.
    [Show full text]
  • In Pdf Format
    lós 1877 Mik 88 ge N 18 e N i h 80° 80° 80° ll T 80° re ly a o ndae ma p k Pl m os U has ia n anum Boreu bal e C h o A al m re u c K e o re S O a B Bo l y m p i a U n d Planum Es co e ria a l H y n d s p e U 60° e 60° 60° r b o r e a e 60° l l o C MARS · Korolev a i PHOTOMAP d n a c S Lomono a sov i T a t n M 1:320 000 000 i t V s a Per V s n a s l i l epe a s l i t i t a s B o r e a R u 1 cm = 320 km lkin t i t a s B o r e a a A a A l v s l i F e c b a P u o ss i North a s North s Fo d V s a a F s i e i c a a t ssa l vi o l eo Fo i p l ko R e e r e a o an u s a p t il b s em Stokes M ic s T M T P l Kunowski U 40° on a a 40° 40° a n T 40° e n i O Va a t i a LY VI 19 ll ic KI 76 es a As N M curi N G– ra ras- s Planum Acidalia Colles ier 2 + te .
    [Show full text]
  • Simulating Martian Regolith in the Laboratory
    ARTICLE IN PRESS Planetary and Space Science 56 (2008) 2009–2025 www.elsevier.com/locate/pss Simulating Martian regolith in the laboratory Karsten Seiferlina,Ã, Pascale Ehrenfreundb, James Garryb, Kurt Gundersona,E.Hu¨tterc, Gu¨nter Karglc, Alessandro Maturillid, Jonathan Peter Merrisone aPhysikalisches Institut, Universita¨t Bern, Sidlerstrasse 5, 3012 Bern, Switzerland bAstrobiology Laboratory, Leiden Institute of Chemistry, P.O. Box 9502, 2300 RA Leiden, The Netherlands cInstitut fu¨r Weltraumforschung, Graz, O¨sterreichische Akademie der Wissenschaften, Austria dGerman Aerospace Centre (DLR), Institute for Planetary Research, Rutherfordstr. 2, 12489 Berlin-Adlershof, Germany eAarhus Mars Simulation Laboratory, Aarhus University, Denmark Received 6 December 2007; received in revised form 21 July 2008; accepted 21 September 2008 Available online 15 October 2008 Abstract Regolith and dust cover the surfaces of the Solar Systems solid bodies, and thus constitute the visible surface of these objects. The topmost layers also interact with space or the atmosphere in the case of Mars, Venus and Titan. Surface probes have been proposed, studied and flown to some of these worlds. Landers and some of the mechanisms they carry, e.g. sampling devices, drills and subsurface probes (‘‘moles’’) will interact with the porous surface layer. The absence of true extraterrestrial test materials in ample quantities restricts experiments to the use of soil or regolith analogue materials. Several standardized soil simulants have been developed and produced and are commonly used for a variety of laboratory experiments. In this paper we intend to give an overview of some of the most important soil simulants, and describe experiments (penetrometry, thermal conductivity, aeolian transport, goniometry, spectroscopy and exobiology) made in various European laboratory facilities.
    [Show full text]
  • List of Licensed Financial Institutions
    LIST OF LICENSED FINANCIAL INSTITUTIONS The Central Bank of Lesotho hereby notifies members of the public that the under-mentioned financial institutions are duly licensed to operate in Lesotho in terms of the Financial Institutions Act of 2012, the Insurance Act of 2014 and Collective Investment Schemes Regulations of 2001. The list includes approved banks, insurance companies, insurance brokers, Micro Finance, Credit Bureau, Foreign Exchange and collective investment schemes. Members of the public who wish to check the list of approved money lenders in Lesotho can call the Central Bank of Lesotho on the following numbers; (+266) 22232039. Members of the public will be kept informed about approved financial institutions on a quarterly basis in order to enable them to avoid investing in un-authorized financial institutions. LIST OF LICENSED COMMERCIAL BANKS AND FOREX AGENCIES NAME OF INSTITUTION NAME OF CHIEF EXECUTIVE OFFICER OR MANAGING DIRECTOR PHYSICAL & POSTAL ADDRESS CONTACTS Standard Lesotho Bank Mr Mpho Vumbukani Head Office, Kingsway Street, P.O. Box 1053, Maseru 100 (+266) 22315737 Nedbank Lesotho Mr Papa Sekyiamah a.i Head Office, Kingsway Street, P.O. Box 1001, Maseru 100 (+266) 22312696 First National Bank Lesotho Mr Bradwin Roper Head Office, Kingsway Street, P.O. Box 11902, Maseru 100 (+266) 22247100 Lesotho Postbank Mr Molefi Leqhaoe Post Office Building, P/B A121, Maseru 100 (+266) 22317842 LIST OF LICENSED INSURANCE COMPANIES NAME OF INSTITUTION PRINCIPAL OFFICER PHYSICAL & POSTAL ADDRESS CONTACT DETAILS Lesotho National Life Assurance Ltd, Life Insurance Mr. Ralitapole J. Letsoela, Managing Director LNGIC House Constitution Road Maseru, Lesotho 100 (+266) 22314144 Alliance Insurance Company Ltd, Life & General Insurance Mr.
    [Show full text]
  • LESOTHO Reference Map
    LESOTHO Reference Map SOUTH AFRICA Makhunoane Liqobong Likila Ntelle n Maisa-Phoka Ts'a-le- o d Moleka le BUTHA BUTHE a Lipelaneng C Nqechane/ Moteng Sephokong Linakeng Maputsoe Leribe Menkhoaneng Sekhobe Litjotjela Likhotola/ LERIBE Hleoheng Malaoaneng Manka/ Likhakeng Matlameng Mapholaneng/ Fobane Koeneng/ Phuthiatsana Kolojane Lipetu/ Kao Pae-la-itlhatsoa -Leribe Fenyane Litsilo -Pae-la-itlhatsoa Mokhachane/ Mamathe/Bulara Mphorosane Molika-liko Makhoroana Limamarela Tlhakanyu/Motsitseng Teyateyaneng Seshote Mapholaneng/ Majoe-Matso/ Meno/ Lekokoaneng/Maqhaka Mohatlane/ Sebetia/Khokhoba Pae-la-itlhatsoa Matsoku -Mapholaneng MOKHOTLONG Lipohong Thuapa-Kubu/ Moremoholo/ Katse Popa Senekane BEREA Moshemong Maseru Thuathe Koali/ Taung/Khubelu Mejametalana p Mokhameleli Semenanyane Mokhotlong S Maluba-lube/ Mateanong e Maseru Suoane/ m Rafolatsane Thaba-Bosiu g Ratau e Liphakoeng n Bokong n e a Ihlo-Letso/ Mazenod Maseru Moshoeshoe l Setibing/ Khotso-Ntso Sehong-hong e Tsoelike/ Moeketsane h Pontseng/ Makopoi/ k Mantsonyane Bobete p Popa_MSU a Likalaneng Mahlong Linakaneng M Thaba-Tseka/ Rothe Mofoka Nyakosoba/Makhaleng Maboloka Linakeng/Bokhoasa/Manamaneng THABA TSEKA Kolo/ MASERU Setleketseng/ Tebang/ Matsieng Tsakholo/Mapotu Seroeneg S Mashai e Boleka n Tsa-Kholo Ramabanta/ q Methalaneng/ Tajane Moeaneng u Rapo-le-boea n Khutlo-se-metsi Litsoeneng/Qalabane Maboloka/ y Sehonghong Thaba-Tsoeu/ Monyake a Lesobeng/ Mohlanapeng Mathebe/ n Sehlaba-thebe/ Thabaneng Ribaneng e Takalatsa Likhoele Moshebi/ Kokome/ MAFETENG Semonkong Leseling/
    [Show full text]