Splendors of Namibia 14 Days / 13 Nights
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Motorcycle Tour South Africa and Namibia, from Cape Town to Windhoek Motorcycle Tour South Africa and Namibia, from Cape Town to Windhoek
Motorcycle tour South Africa and Namibia, from Cape Town to Windhoek Motorcycle tour South Africa and Namibia, from Cape Town to Windhoek Duração Dificuldade Veículo de apoio 14 días Normal-Hard Sim Language Guia en,de Sim Namibia, a vast 830 thousand square kilometre expense of desert flanked by the icy Atlantic Ocean, is home to slightly less than 1.7 million citizens. That’s less than half the number of Cape Town residents. Unending roads stretch out as far as the eye can see under a sky that’s so big it can only be described as heavenly with space enough to truly breathe. The two-week trip starts in Cape Town and winds its way up our west coast to culminate in Namibia’s capital, Windhoek. With both on and off-road riding, the 2,100 miles city to city tour is an epic tribute to solitude and uninterrupted riding with out-of-this world scenery. Your on-road riding experience will be punctuated by some gravel road riding exploring such places as the mountainous Cedarberg region, the Northern Cape, one of the world’s oldest deserts as well as the Fish River Canon, the world’s second largest canyon. Approximately 50% of this tour is on dirt roads, some basic off-road riding skills are required. Itinerário 1 - - Cidade do Cabo - 0 Welcome. Almost all international flights arrive in Cape Town before midday. Our tour guide will meet you at the airport and taxi you directly to your hotel where you can freshen-up and perhaps have a light bite to eat. -
One of Five West Coast, Low-Latitude Deserts of the World, the Namib Extends Along the Entire Namibian Coastline in an 80-120 Km Wide Belt
N A M I B I A G 3 E 0 O 9 1 L - O Y G E I V C R A U S L NAMIB DESERT Source: Roadside Geology of Namibia One of five west coast, low-latitude deserts of the world, the Namib extends along the entire Namibian coastline in an 80-120 km wide belt. Its extreme aridity is the result of the cold, upwelling Benguela Current, which flows up the west coast of Africa as far as Angola, and because of its low temperatures induces very little evaporation and rainfall (<50 mm per year). It does, however, create an up to 50 km wide coastal fog belt providing sufficient moisture for the development of a specialist flora and fauna, many of which are endemic to the Namib. In addition, the lagoons at Walvis Bay and Sandwich Harbour are designated wetlands of international importance, because of their unique setting and rich birdlife, including flamingo, white pelican and Damara tern. Larger mammals like the famed desert elephant, black rhino, lion, cheetah and giraffe can be found along the northern rivers traversing the Skeleton Coast National Park. Geomorphologically, the Namib includes a variety of landscapes, including classic sand dunes, extensive gravel plains, locally with gypcrete and calcrete duricrusts, elongated salt pans, ephemeral watercourses forming linear oases, inselbergs and low mountain ranges. Along the coast, wind-swept sandy beaches alternate with rocky stretches, in places carved into striking rock formations (e.g. Bogenfels Arch). Designated a UNESCO World Heritage Site in 2013, the “Namib Sand Sea“ between Lüderitz and the Kuiseb River encompasses such well-known landmarks as Sossusvlei and Sandwich Harbour, while the fabled Skeleton Coast north of the Ugab River is notorious for its numerous ship wrecks. -
NAMIBIA Angola, Zambia,Namibia,Botswana,Zimbabweandsouthafrica
© Lonely Planet Publications 304 lonelyplanet.com NAMIBIA •• Highlights 305 extreme sports in Swakopmund ( p360 ), N a m i b i a HOW MUCH? take a safari through Etosha ( p332 ), hike Dune surfing US$25 the Fish River Canyon ( p385 ) and go on an exped ition through the northwest and Foreign newspaper US$1.70 along the Skele ton Coast ( p354 ). Night in a budget hotel US$12.50 Package of kudu biltong US$1 CLIMATE & WHEN TO GO Traditional German dinner US$6 Namibia’s climatic variations correspond Wedged between the Kalahari and the South Atlantic, Namibia enjoys both vast potential roughly to its geographical subdivisions. In and promise as one of the youngest countries in Africa. In addition to a striking diversity LONELY PLANET INDEX the arid Central Namib, summer daytime of cultures and national origins, Namibia is also a photographer’s dream – it boasts wild temperatures may climb to over 40°C, but seascapes, rugged mountains, lonely deserts, stunning wildlife, colonial cities and nearly 1L of petrol US$0.75 can fall to below freezing during the night. Rainfall is heaviest in the northeast, which unlimited elbow room. 1L of bottled water US$0.50-1 enjoys a subtropical climate, and along the Bottle of beer US$1 A predominantly arid country, Namibia can be divided into four main topographical re- Okavango River, rainfall reaches over 600mm Souvenir T-shirt US$5-10 annually. The northern and interior regions gions: the Namib Desert and coastal plains in the west, the eastward-sloping Central Plateau, Snack US$1-2 experience the ‘little rains’ between October the Kalahari along the borders with South Africa and Botswana, and the densely wooded and December, while the main stormy period bushveld of the Kavango and Caprivi regions. -
Gletscherkunde Late Quaternary Development
Band 21 (1985), S. 151-157 ZEITSCHRIFT FÜR GLETSCHERKUNDE UND GLAZIALGEOLOGIE © 1985 by Universitätsverlag Wagner, Innsbruck LATE QUATERNARY DEVELOPMENT OF THE KUISEB RIVER VALLEY AND ADJACENT AREAS, CENTRAL NAMIB DESERT, SOUTH WEST AFRICA/NAMIBIA, AND PALAEOCLIMATIC IMPLICATIONS By K. HEINE, Regensburg With 3 figures SUMMARY A chronology of climatic change in the central Namib desert may be reconstructed, based upon geomorphological and stratigraphical relationships and absolute dating of fluvial sequences, and upon speleothem development and dating. Correlation of events between the Kui- seb valley and Rössing Cave reveals the following pattern of Late Quaternary palaeoenviron- ments: (1) Wetter than today from > 40,500 to 34,000/33,000 BP, (2) Alternating arid/windy and moist from 34,000/33,000 to 27,000 BP, (3) Between 27,000 and 25,500 BP wetter than today, (4) Since 25,500 BP arid (with several short periods of somewhat moister conditions locally, dur• ing the Holocene). (5) Extremely arid since 600/500 BP. DIE JUNGQUARTÄRE ENTWICKLUNG DES KUISEBTALES UND ANGRENZENDER GEBIETE, ZENTRALE NAMIB, SÜDWESTAFRIKA/NAMIBIA, UND PALÄOKLIMATISCHE FOLGERUNGEN ZUSAMMENFASSUNG Für die zentrale Namib kann eine Chronologie der Paläoklimate rekonstruiert werden, wenn nicht allein die geomorphologischen und stratigraphischen Beziehungen und absoluten Datie• rungen der fluvialen Abfolgen, sondern darüber hinaus Höhlensinterbildung und -datierung hin• zugezogen werden. Die Korrelierung der Ereignisse des Kuisebtales mit denen der Rössing- Höhle erlaubt folgende Aussagen: (1) Feuchter als heute von > 40,500 bis 34,000/33,000 BP, (2) Alternierend arid/windig und feucht von 34,000/33,000 bis 27,000 BP, (3) Zwischen 27,000 und 25,500 BP feuchter als heute, (4) Seit 25,500 arid (mit einigen kurzen holozänen Perioden mit etwas feuchteren Bedingungen, jedoch nur von lokaler Bedeutung). -
Touring Katutura! : Poverty, Tourism, and Poverty Tourism In
Universität Potsdam Malte Steinbrink | Michael Buning | Martin Legant | Berenike Schauwinhold | Tore Süßenguth TOURING KATUTURA ! Poverty, Tourism, and Poverty Tourism in Windhoek, Namibia Potsdamer Geographische Praxis // 11 Potsdamer Geographische Praxis Potsdamer Geographische Praxis // 11 Malte Steinbrink|Michael Buning|Martin Legant| Berenike Schauwinhold |Tore Süßenguth TOURING KATUTURA! Poverty, Tourism, and Poverty Tourism in Windhoek, Namibia Universitätsverlag Potsdam Bibliografische Information der Deutschen Nationalbibliothek Die Deutsche Nationalbibliothek verzeichnet diese Publikation in der Deutschen Nationalbibliografie; detaillierte bibliografische Daten sind im Internet über http://dnb.dnb.de/ abrufbar. Universitätsverlag Potsdam 2016 http://verlag.ub.uni-potsdam.de Am Neuen Palais 10, 14469 Potsdam Tel.: +49 (0)331 977 2533 / Fax: -2292 E-Mail: [email protected] Die Schriftenreihe Potsdamer Geographische Praxis wird herausgegeben vom Institut für Geographie der Universität Potsdam. ISSN (print) 2194-1599 ISSN (online) 2194-1602 Das Manuskript ist urheberrechtlich geschützt. Gestaltung: André Kadanik, Berlin Satz: Ute Dolezal Titelfoto: Roman Behrens Druck: docupoint GmbH Magdeburg ISBN 978-3-86956-384-8 Zugleich online veröffentlicht auf dem Publikationsserver der Universität Potsdam: URN urn:nbn:de:kobv:517-opus4-95917 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-95917 CONTENT 1 INTRODUCTION ........................................................................................ 11 1.1 Background of the study: -
Title: Walvis Bay Baseline Study *By: Priscilla Rowswell and Lucinda Fairhurst *Report Type: Research Study, *Date: February 2011
ICLEI – Local Governments for Sustainability – Africa Walvis Bay Baseline Study *Title: Walvis Bay Baseline Study *By: Priscilla Rowswell and Lucinda Fairhurst *Report Type: Research Study, *Date: February 2011 *IDRC Project Number-Component Number: 105868-001 *IDRC Project Title: Sub-Saharan African Cities: A Five-City Network to Pioneer Climate Adaptation through Participatory Research and Local Action. *Country/Region: Namibia, South Africa, Mozambique, Tanzania, Mauritius *Full Name of Research Institution: ICLEI – Local Governments for Sustainability - Africa *Address of Research Institution: P.O. Box 5319, Tygervalley, 7536, Cape Town, South Africa *Name(s) of ICLEI Africa Core Project Team: Lucinda Fairhurst and Priscilla Rowswell *Contact Information of Researcher/Research Team members: [email protected]; +27 21 487 2312 *This report is presented as received from project recipient(s). It has not been subjected to peer review or other review processes. *This work is used with the permission of ICLEI – Local Governments for Sustainability - Africa *Copyright: 2012, ICLEI – Local Governments for Sustainability - Africa *Abstract: This project addresses knowledge, resource, capacity and networking gaps on the theme: 'Strengthening urban governments in planning adaptation.' The main objective of this project is to develop an adaptation framework for managing the increased risk to African local government and their communities due to climate change impact. The ultimate beneficiaries of this project will be African local governments and their communities. The guiding and well-tested ICLEI principle of locally designed and owned projects for the global common good, specifically in a developing world context, will be applied throughout project design, inception and delivery. Additionally, the research will test the theory that the most vulnerable living and working in different geographical, climatic and ecosystem zones will be impacted differently and as such, will require a different set of actions to be taken. -
Mcmenamin FM
The Garden of Ediacara • Frontispiece: The Nama Group, Aus, Namibia, August 9, 1993. From left to right, A. Seilacher, E. Seilacher, P. Seilacher, M. McMenamin, H. Luginsland, and F. Pflüger. Photograph by C. K. Brain. The Garden of Ediacara • Discovering the First Complex Life Mark A. S. McMenamin C Columbia University Press New York C Columbia University Press Publishers Since 1893 New York Chichester, West Sussex Copyright © 1998 Columbia University Press All rights reserved Library of Congress Cataloging-in-Publication Data McMenamin, Mark A. The garden of Ediacara : discovering the first complex life / Mark A. S. McMenamin. p. cm. Includes bibliographical references and index. ISBN 0-231-10558-4 (cloth) — ISBN 0–231–10559–2 (pbk.) 1. Paleontology—Precambrian. 2. Fossils. I. Title. QE724.M364 1998 560'.171—dc21 97-38073 Casebound editions of Columbia University Press books are printed on permanent and durable acid-free paper. Printed in the United States of America c 10 9 8 7 6 5 4 3 2 1 p 10 9 8 7 6 5 4 3 2 1 For Gene Foley Desert Rat par excellence and to the memory of Professor Gonzalo Vidal This page intentionally left blank Contents Foreword • ix Preface • xiii Acknowledgments • xv 1. Mystery Fossil 1 2. The Sand Menagerie 11 3. Vermiforma 47 4. The Nama Group 61 5. Back to the Garden 121 6. Cloudina 157 7. Ophrydium 167 8. Reunite Rodinia! 173 9. The Mexican Find: Sonora 1995 189 10. The Lost World 213 11. A Family Tree 225 12. Awareness of Ediacara 239 13. Revenge of the Mole Rats 255 Epilogue: Parallel Evolution • 279 Appendix • 283 Index • 285 This page intentionally left blank Foreword Dorion Sagan Virtually as soon as earth’s crust cools enough to be hospitable to life, we find evidence of life on its surface. -
Ai-/Ais-Richtersveld Transfrontier Park “Since This Spectacular Area Is Undeveloped and There Is So Much to Explore, You Feel As If No One Else Has Ever Been Here
/Ai-/Ais-Richtersveld Transfrontier Park “Since this spectacular area is undeveloped and there is so much to explore, you feel as if no one else has ever been here. That the park is yours alone to discover.” Wayne Handley, Senior Ranger, /Ai-/Ais Richtersveld Republic of Namibia Transfrontier Park, Ministry of Environment and Tourism Ministry of Environment and Tourism Discover the /Ai-/Ais Richtersveld 550 metres above. Klipspringer bound up the cliffs and moun- Transfrontier Park tain chats drink from pools left behind from when the river last Experience wilderness on a scale unimaginable. Stand at the edge flowed. Ancient rock formations and isolation add to the sense of of the largest natural gorge in Africa, and the second-largest can- timelessness and elation that mark this challenging hike. yon in the world, the Fish River Canyon. Revel in the dramatic views from Hell’s Corner where it is almost possible to imagine For 4x4 enthusiasts, drives along the rugged eastern rim of the the dramatic natural forces that shaped the canyon. Today the canyon afford stunning views across the canyon from Hell’s /Ai-/Ais Richtersveld Transfrontier Park protects a vast area that Corner and Sulphur Springs vantage points. One hundred ki- crosses the South African border to encompass one of the richest lometres further south, another more leisurely route winds botanical hot spots in the world, the Succulent Karoo biome. along the edge of the Orange River, where masses of water are framed by towering black mountains. Strewn with immense boulders, the bed of the Fish River is also home to one of the most exhilarating adventures in Southern Everywhere there are rare plants, including 100 endemic suc- Africa, the five-day, 90-kilometre Fish River Canyon hiking trail, culents and over 1 600 other plant species, illusive rare animals, for which you need a hiking permit. -
Managing Biodiversity of the Greater Fish River Canyon Landscape
Managing biodiversity of the Greater Fish River Canyon Landscape A tool for sustainable land management Managing biodiversity of the Greater Fish River CanyonCanyon Landscape A tool for sustainable land management Antje Burke NNNovemberNovember 2012013333 1 © Antje Burke, 2013 This publication may be reproduced for non-commercial purposes only. Content and design: Antje Burke Published in 2013 by EnviroScience PO Box 90230 Klein Windhoek Namibia And Namibia Protected Landscape Conservation Areas Initiative (NAM-PLACE) Ministry of Environment and Tourism Private Bag 13306 Windhoek Namibia Suggested citation: Burke, A. (2013) Managing biodiversity of the Greater Fish River Canyon Landscape - A tool for sustainable land management. EnviroScience and Namplace, Windhoek, 92 pp. Acknowledgements This survey would have been impossible without the enthusiastic support of all GFRCL stakeholders and Namplace’s financial and logistic support. Not only the stakeholders whose properties we needed to access, but also those were no data gaps were identified, were eager to support us. We are therefore sorry that we did not have the time to visit all farms. Leevi’s assistance was essential to ensure that good specimens of critical species are lodged at the National Botanical Research Institute and that the taxing work in the mountain areas could be undertaken safely. Coleen Mannheimer deserves special thanks for volunteering her time freely and helping with the (often tedious) plant identifications. Jonas Heita ensured that stakeholders were well briefed and put me in contact with right people. In the field, we (Leevi and I) would particularly like to thank Eben Naude, Liana Mbako, Simon Goliath, Sikongo Ignatius Nyangana (Gammy), Reagan Mbeava, Max Witbooi, Mnh Dekoker, Angela Otseeng, Tryg and Sue Cooper and Manni Goldbeck and his staff at the Canyon village. -
Neogene and Quaternary Vertebrate Biochronology of the Sperrgebiet
Communs geol. Surv. Namibia, 12 (2000), 411-419 Neogene and Quaternary vertebrate biochronology of the Sperrgebiet and Otavi Mountainland, Namibia Martin Pickford Chaire de Paléoanthropologie et de Préhistoire Collège de France and Laboratoire de Paléontologie, UMR 8569 du CNRS 8, rue Buffon, 75005, Paris e-mail >[email protected]< Since 1991, the Namibia Palaeontology Expedition has discovered well over 100 fossiliferous localities in Namibia which have provided useful biochronological data. The Otavi karst field has yielded fossiliferous breccias which span the period from late Mid- dle Miocene (ca 13 Ma) to Recent. At several vanadium occurrences, including Berg Aukas and Harasib 3a, it is clear that vanadium mineralisation occurred during the Miocene, whereas at others, such as Rietfontein, mineralisation was taking place as recently as the Pleistocene. The only substantial vanadium deposit that remains undated is Abenab. The diamondiferous proto-Orange terrace deposits are now known to span the period early Miocene to basal Middle Miocene (Auchas, Arrisdrift) while the meso-Orange terraces are of Late Miocene and Plio-Pleistocene age. The raised beach deposits north of Oranjemund are older than previously thought, the earliest (50 m beach) dating from the Pliocene while the youngest ones (sub-10m beaches) are of Late Pleistocene to Recent age. There are boul- ders in some of the beach deposits at Oranjemund that may well represent reworked material from the 90 metre beach, although in situ deposits of this age have not been found in Namibia. The onset of desertification in the Namib dates from the end of the Early Miocene, some 17 Ma. -
Kuiseb Basin Water Resources Management Project
File Number: 12/13/5/2/4 REPUBLIC OF NAMIBIA MINISTRY OF AGRICULTURE, WATER AND FORESTRY DEPARTMENT OF WATER AFFAIRS AND FORESTRY Kuiseb Basin Water Resources Management Project - Development of a Water Resources Plan for the Kuiseb Basin and Development of a Planning Procedure for use by Other Basins - Part GEOHYDROLOGY GEOHYDROLOGY DIVISION COMPILED BY: DEPARTMENT OF WATER AFFAIRS Dr. Martin Falke PRIVATE BAG 13193 CIM-Consultant WINDHOEK July 2008 Geo-hydrology ii Table of Contents 1 BASELINE INFORMATION AND GAPS ANALYSIS CONCERNING GEOLOGY AND GEOHYDROLOGY OF THE BASIN 4 1.1 Inventory of relevant geological and geo-hydrological records and reports 4 1.2 Overviews of Main Hydrological & Geological Features 6 1.2.1 Hydrology 6 1.2.2 Geology 7 1.2.3 Main Aquifer Types 7 1.3 Groundwater-Dependant Ecosystems (see also B 7 & B 8) 9 1.4 Gaps and shortcomings in information, knowledge and measures 9 2 WATER RESOURCES 9 2.1 Inventory of relevant records and reports of presently used groundwater sources and unutilised groundwater resources 9 2.2 Concise description of these features/resources, including undeveloped water resource potential 10 2.3 Recharge dynamics and rates, discharge, abstractions and the possible over-exploitation of groundwater 13 2.4 Future water requirements for mining activities in the Kuiseb Basin 15 2.5 Concise description concerning health of groundwater resources and the threats thereto, including quality and pollution of these waters, in order to devise control, protection and remedial measures 16 2.5.1 Groundwater -
8D7N Best of Nambia
0 Windhoeekk –– SossusvleiSossusvlei –– Walvisalvis BayBay –– SwakopmundSwakopmund –– Windhoekk Namib Desert, Sossuslei MINIMUM 4 ADULTS Season Twin Share Single Room Supplement January - June 11,950 1,820 July – November 12,260 1,890 December 12,510 1,960 PRICE INCLUSIONS Return airport-hotel-airport transfer Day City Hotel/Lodge (or similar class) 07 Nights hotel accommodation with 01 Windhoek Avani Windhoek Hotel & Casino daily breakfast 02 Kalahari Desert Lapa Lange Lodge Service of an English speaking driver cum 03 & 04 Sossuslei Area Le Mirage Resort & Spa guide 05 & 06 Walvis Bay Lagoon Flamingo Villas Boutique Hotel Lunch and dinner as specified in the 07 Windhoe Avani Windhoek Hotel & Casino itinerary Bottled mineral water daily DAY ITINERARY Med Emergency Rescue and Evacuation 01 WINDHOEK – ARRIVAL (D) within Namibia Arrived at Windhoek Airport, meet and greet by local representative and transfer to Value Added Tax Tourism Levy hotel for check in. PRICE EXCLUSIONS 02 WINDHOEK – MARIENTAL (B/L/D) International airfare Morning depart south to Kalahari Desert. Afternoon nature Sundowner Drive. After Applicable airport taxes dinner enjoy the clear night skies with star gazing (subject to weather condition). Personal Incidental Expenses Travel Insurance 03 MARIENTAL – SOSSUSVLEI (B/L/D) Gratuities to guide & driver : Morning walk with SAN Bushman family. Later depart to Namib Desert en-route visit US$20 per person per day – pay direct the Duwisib Castle. Arrive at Sossusvlei and check in hotel. Evening Sunset Quad REMARKS Bike Trip. Tour prices quoted are subject to change 04 SOSSUSVLEI (B/L/D) with or without prior notice Visit Dunes at Sossusvlei, Dead Vlei, Dune45 & Sesriem Canyon Subject to availability upon making reservation 05 SOSSUSVLEI – WALVIS BAY (B/L/D) No refund for un-utilized tours or services Cross the Tropic of Capricorn through the Kuiseb Pass , Kuiseb Canyon, the Moon Terms & Conditions Apply Landscape and the Welwitschia Plains.