The Pungwe, Buzi, and Save (Pubusa)
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Mozambique Zambia South Africa Zimbabwe Tanzania
UNITED NATIONS MOZAMBIQUE Geospatial 30°E 35°E 40°E L a k UNITED REPUBLIC OF 10°S e 10°S Chinsali M a l a w TANZANIA Palma i Mocimboa da Praia R ovuma Mueda ^! Lua Mecula pu la ZAMBIA L a Quissanga k e NIASSA N Metangula y CABO DELGADO a Chiconono DEM. REP. OF s a Ancuabe Pemba THE CONGO Lichinga Montepuez Marrupa Chipata MALAWI Maúa Lilongwe Namuno Namapa a ^! gw n Mandimba Memba a io u Vila úr L L Mecubúri Nacala Kabwe Gamito Cuamba Vila Ribáué MecontaMonapo Mossuril Fingoè FurancungoCoutinho ^! Nampula 15°S Vila ^! 15°S Lago de NAMPULA TETE Junqueiro ^! Lusaka ZumboCahora Bassa Murrupula Mogincual K Nametil o afu ezi Namarrói Erego e b Mágoè Tete GiléL am i Z Moatize Milange g Angoche Lugela o Z n l a h m a bez e i ZAMBEZIA Vila n azoe Changara da Moma n M a Lake Chemba Morrumbala Maganja Bindura Guro h Kariba Pebane C Namacurra e Chinhoyi Harare Vila Quelimane u ^! Fontes iq Marondera Mopeia Marromeu b am Inhaminga Velha oz P M úngu Chinde Be ni n è SOFALA t of ManicaChimoio o o o o o o o o o o o o o o o gh ZIMBABWE o Bi Mutare Sussundenga Dondo Gweru Masvingo Beira I NDI A N Bulawayo Chibabava 20°S 20°S Espungabera Nova OCE A N Mambone Gwanda MANICA e Sav Inhassôro Vilanculos Chicualacuala Mabote Mapai INHAMBANE Lim Massinga p o p GAZA o Morrumbene Homoíne Massingir Panda ^! National capital SOUTH Inhambane Administrative capital Polokwane Guijá Inharrime Town, village o Chibuto Major airport Magude MaciaManjacazeQuissico International boundary AFRICA Administrative boundary MAPUTO Xai-Xai 25°S Nelspruit Main road 25°S Moamba Manhiça Railway Pretoria MatolaMaputo ^! ^! 0 100 200km Mbabane^!Namaacha Boane 0 50 100mi !\ Bela Johannesburg Lobamba Vista ESWATINI Map No. -
Water Scenarios for the Zambezi River Basin, 2000 - 2050
Water Scenarios for the Zambezi River Basin, 2000 - 2050 Lucas Beck ∗ Thomas Bernauer ∗∗ June 1, 2010 Abstract Consumptive water use in the Zambezi river basin (ZRB), one of the largest fresh- water catchments in Africa and worldwide, is currently around 15-20% of total runoff. This suggests many development possibilities, particularly for irrigated agriculture and hydropower production. Development plans of the riparian countries indicate that con- sumptive water use might increase up to 40% of total runoff already by 2025. We have constructed a rainfall–runoff model for the ZRB that is calibrated on the best available runoff data for the basin. We then feed a wide range of water demand drivers as well as climate change predictions into the model and assess their implications for runoff at key points in the water catchment. The results show that, in the absence of effective international cooperation on water allocation issues, population and economic growth, expansion of irrigated agriculture, and water transfers, combined with climatic changes are likely to have very important transboundary impacts. In particular, such impacts involve drastically reduced runoff in the dry season and changing shares of ZRB coun- tries in runoff and water demand. These results imply that allocation rules should be set up within the next few years before serious international conflicts over sharing the Zambezi’s waters arise. Keywords: Water demand scenarios, Zambezi River Basin, water institutions ∗[email protected] and [email protected], ETH Zurich, Center for Comparative and Interna- tional Studies and Center for Environmental Decisions, Weinbergstrasse 11, 8092 Zurich, Switzerland, Phone: +41 44 632 6466 ∗∗We are very grateful to Tobias Siegfried, Wolfgang Kinzelbach, and Amaury Tilmant for highly useful comments on previous versions of this paper. -
Ecological Changes in the Zambezi River Basin This Book Is a Product of the CODESRIA Comparative Research Network
Ecological Changes in the Zambezi River Basin This book is a product of the CODESRIA Comparative Research Network. Ecological Changes in the Zambezi River Basin Edited by Mzime Ndebele-Murisa Ismael Aaron Kimirei Chipo Plaxedes Mubaya Taurai Bere Council for the Development of Social Science Research in Africa DAKAR © CODESRIA 2020 Council for the Development of Social Science Research in Africa Avenue Cheikh Anta Diop, Angle Canal IV BP 3304 Dakar, 18524, Senegal Website: www.codesria.org ISBN: 978-2-86978-713-1 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording or any information storage or retrieval system without prior permission from CODESRIA. Typesetting: CODESRIA Graphics and Cover Design: Masumbuko Semba Distributed in Africa by CODESRIA Distributed elsewhere by African Books Collective, Oxford, UK Website: www.africanbookscollective.com The Council for the Development of Social Science Research in Africa (CODESRIA) is an independent organisation whose principal objectives are to facilitate research, promote research-based publishing and create multiple forums for critical thinking and exchange of views among African researchers. All these are aimed at reducing the fragmentation of research in the continent through the creation of thematic research networks that cut across linguistic and regional boundaries. CODESRIA publishes Africa Development, the longest standing Africa based social science journal; Afrika Zamani, a journal of history; the African Sociological Review; Africa Review of Books and the Journal of Higher Education in Africa. The Council also co- publishes Identity, Culture and Politics: An Afro-Asian Dialogue; and the Afro-Arab Selections for Social Sciences. -
Letter of Concern: Mining in the Lower Zambezi River Water Catchment and Protected Areas
Letter of Concern: Mining in the Lower Zambezi River Water Catchment and Protected Areas INTRODUCTION This petition is submitted to express the growing concern by the traditional residents of the Lower Zambezi Valley, the international conservation community, and local leaseholders in regard to the numerous proposed mining projects currently under development in the area. These projects are likely to impact the area’s irreplaceable eco-system and cause irreversible damage to one of the greatest natural heritage areas in Zambia, and all of Africa. The mining projects are located both within and adjacent to the Lower Zambezi National Park, the recently formed Partnership Park (the first of its kind in Zambia which is a partnership between community and GMA leaseholders), and Mana Pools National Park, a World Heritage Site located directly across the river in neighboring Zimbabwe. The area currently supports many communities in which thousands of local people depend on sustainable industries including agriculture, fisheries and tourism. As per the signatories document attached, you will see many of the communities are represented here. All of these communities and sustainable enterprises are under threat by the potential consequences of the proposed mining, which does not provide long-term economic benefits to Zambian citizens. As a unique and world-renowned ecosystem with immense financial and ecological value to Zambia, this area deserves the highest level of protection. We are very concerned about the profound and long- lasting negative socio-economic and environmental impacts that are likely to occur if the proposed mining operations go forward. The proposed open pit mining projects are located inside the Zambezi River water catchment, in close proximity to tributaries to this invaluable water resource. -
Southern Africa • Floods Regional Update # 5 20 April 2010
Southern Africa • Floods Regional Update # 5 20 April 2010 This report was issued by the Regional Office for Southern and Eastern Africa (ROSEA). It covers the period from 09 to 20 April 2010. The next report will be issued within the next two weeks. I. HIGHLIGHTS/KEY PRIORITIES • An assessment mission to the Angolan Province of Cunene found that 23,620 people have been affected by floods; • In Madagascar, access to affected communities remains an issue. II. Regional Situation Overview As the rainy season draws to a close, countries downstream of the Zambezi River - Malawi, Mozambique, Zambia and Zimbabwe – are not experiencing any new incidences of flooding. However, continuing high water levels in the upper Zambezi, Cunene, Cuvelai and Kavango Rivers are still being recorded, affecting Angola and northern Namibia. Furthermore, as the high water levels in the upper Zambezi River move downstream, localized flooding remains a possibility. In the next two weeks, no significant rainfall is expected over the currently flood-affected areas or their surrounding basins. III. Angola A joint assessment mission by Government and the United Nations Country Team (UNCT) was conducted in the flood-affected Cunene Province from 06 to 09 April 2010. The mission found that 23,620 people (3,300 households) have been affected by floods in the province. Of that total, 12,449 people (1,706 households) have been left homeless but have been able to stay with neighbors and family, whilst the remaining 11,171 people (1,549 households) have been relocated to Government-managed camps within the province. There are also reports of damage to schools and infrastructure. -
Mozambique Case Study Example1
Mozambique Case study example1 - Principle 1: The Zambezi River Basin - "dialogue for building a common vision" The Zambezi River Basin encompasses some 1.300 km2 throughout the Southern African Development Community (SADC) region, including a dense network of tributaries and associated wetland systems in eight countries (Angola, Namibia, Botswana, Zimbabwe, Zambia, Malawi, Tanzania, Mozambique). The livelihoods of approximately 26 million people are directly dependent on this basin, deriving benefits from its water, hydro-electric power, irrigation developments, fisheries and great wealth of related natural resources, including grazing areas, wildlife, and tourism. Over the past forty years, however, the communities and ecosystems of the lower Zambezi have been constraint by the management of large upstream dams. The toll is particularly high on Mozambique, as it the last country on the journey of the Zambezi; Mozambicans have to live with the consequences of upriver management. By eliminating natural flooding and greatly increasing dry season flows in the lower Zambezi, Kariba Dam (completed in 1959) and especially Cahora Bassa Dam (completed in 1974) cause great hardship for hundreds of thousands of Mozambican villagers whose livelihoods depend on the ebb and flow of the Zambezi River. Although these hydropower dams generate important revenues and support development however, at the expense of other resource users. Subsistence fishing, farming, and livestock grazing activities have collapsed with the loss of the annual flood. The productivity of the prawn fishery has declined by $10 - 20 million per year -- this in a country that ranks as one of the world’s poorest nations (per capita income in 2000 was USD230). -
Dynamic Evolution of the Zambezi-Limpopo Watershed, Central Zimbabwe
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Online Research @ Cardiff Moore, Blenkinsop and Cotterill Zim watershed_20120408_AEM DYNAMIC EVOLUTION OF THE ZAMBEZI-LIMPOPO WATERSHED, CENTRAL ZIMBABWE Andy Moore1,2, Tom Blenkinsop3 and Fenton (Woody) Cotterill4 1African Queen Mines Ltd., Box 66 Maun, Botswana. 2Dept of Geology, Rhodes University, Grahamstown 6140, South Africa. Email: [email protected] 3School of Earth and Environmental Sciences, James Cook University, Townsville, QLD4811, Australia. Email: [email protected] 4AEON – African Earth Observatory Network, Geoecodynamics Research Hub, University of Stellenbosch, Private Bag X1, Matieland 7602, South Africa. Email: [email protected] ABSTRACT Prospecting carried out to the south of the Zambezi-Limpopo drainage divide in the vicinity of Bulawayo, Zimbabwe, led to the recovery of a suite of ilmenites with a chemical “fingerprint” that can be closely matched with the population found in the early Palaeozoic Colossus kimberlite, which is located to the north of the modern watershed. The ilmenite geochemistry eliminates other Zimbabwe Kimberlites as potential sources of these pathfinder minerals. Geophysical modelling has been used to ascribe the elevation of southern Africa to dynamic topography sustained by a mantle plume; however, the evolution of the modern divide between the Zambezi and Limpopo drainage basins is not readily explained in terms of this model. Rather, it can be interpreted to represent a late Palaeogene continental flexure, which formed in response to crustal shortening, linked to intra-plate transmission of stresses associated with an episode of spreading reorganization at the ocean ridges surrounding southern Africa. -
Mozambique Suffers Under Poor WASH Facilities and Is Prone MOZAMBIQUE to Outbreaks of Water- and Vector-Borne Diseases
ACAPS Briefing Note: Floods Briefing Note – 26 January 2017 Priorities for WASH: Provision of drinking water is needed in affected areas. humanitarian Mozambique suffers under poor WASH facilities and is prone MOZAMBIQUE to outbreaks of water- and vector-borne diseases. intervention Floods in central and southern provinces Shelter: Since October 2016, 8,162 houses have been destroyed and 21,000 damaged by rains and floods. Health: Healthcare needs are linked to the damage to Need for international Not required Low Moderate Significant Major healthcare facilities, which affects access to services. At least assistance X 30 healthcare centres have been affected. Very low Low Moderate Significant Major Food: Farmland has been affected in Sofala province, one of Expected impact X the main cereal-producing areas of a country where 1.8 million people are already facing Crisis (IPC Phase 3) levels of food Crisis overview insecurity. Since the beginning of January 2017, heavy seasonal rains have been affecting central Humanitarian Several roads and bridges have been damaged or flooded in the and southern provinces in Mozambique. 44 people have died and 79,000 have been constraints affected provinces. Some areas are only accessible by boat, and affected. The Mozambican authorities issued an orange alert for the provinces of aid has to be airdropped. Maputo, Gaza, Inhambane and Nampula, yet areas of Tete and Sofala provinces have also been affected. The orange alert means that government institutions are planning for an impending disaster. Continued rainfall has been forecasted for the first quarter of 2017. Key findings Anticipated The impact will be influenced by the capacity of the government to respond. -
Primary Solidarities and the Colonial Past in Mozambique VIBRANT - Vibrant Virtual Brazilian Anthropology, Vol
VIBRANT - Vibrant Virtual Brazilian Anthropology E-ISSN: 1809-4341 [email protected] Associação Brasileira de Antropologia Brasil de Pina-Cabral, João Listing Rivers and Train Stations: Primary Solidarities and the Colonial Past in Mozambique VIBRANT - Vibrant Virtual Brazilian Anthropology, vol. 2, núm. 1-2, diciembre, 2005, pp. 27-53 Associação Brasileira de Antropologia Brasília, Brasil Available in: http://www.redalyc.org/articulo.oa?id=406941900003 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative 27 Listing Rivers and Train Stations: Primary Solidarities and the Colonial Past in Mozambique João de Pina-Cabral 1 Summary In understanding present-day Mozambique, stress is usually placed on the colonial/postcolonial temporal boundary as a foundational moment. Colonialism, socialist post colonialism and the present capitalist period appear to annul each other in succession through a chain of successive acts of overcoming. This paper argues that this gives rise to a number of incongruities, for it hides the way in which social persons are linked to historical processes via their primary solidarities. The past and the present are constantly being re-mixed into conglomerates of experience, where each component becomes largely indissociable from the others. The past and the present constantly visit each other in human experience. It is argued that only thus can one make sense of the claims to elite status that are witnessed today. 1 Institute of Social Sciences,University of Lisbon,October 2004. -
Zimbabwe Livelihood Zone Profiles. December 2010
Zimbabwe Livelihoods Zone VAC ZIMBABWE Profiles Vulnerability Assessment Committee 15 February 2010 The Zimbabwe Vulnerability Assessment Committee (ZimVac) is Chaired by the Food and Nutrition Council (FNC) which is housed at the Scientific Industrial Research and Developing Council (SIRDC), Harare, Zimbabwe. Acknowledgements The Zimbabwe Vulnerability Assessment Committee (ZimVac) would like to express its appreciation for the financial, technical and logistical support that the following agencies provided towards the data collection, analysis and writing-up of the Revised Livelihoods profiles for Zimbabwe; Ministry of Agriculture, Irrigation Development and Mechanizations’ Department of Agricultural Extension Services (AGRITEX) Ministry of Labour and Social Welfare’s Department of Social Welfare Ministry of Finance’s Central Statistical Office (CSO) Ministry of Education’s Curriculum Development Ministry of Transport’s Department of Meteorological Services United Nations’ World Food Programme (WFP) United Nations’ Food and Agriculture Organization (FAO) United Nations’ Office of Coordination of Humanitarian Affairs (OCHA) World Vision (WV) OXFAM ACTIONAID Save the Children United Kingdom (SC-UK) Southern Africa Development Community Regional Vulnerability Assessment Committee (RVAC) United States of America International Development Agency (USAID) Department for International Development (DFID) The European Commission (EC) FEG (The Food Economy Group) The Famine Early Warning Systems Network (FEWSNET) The revision -
High Potential in the Lower Zambezi
2 High Potential in the Lower Zambezi A way forward to sustainable development Version 1.0 High Potential in the Lower Zambezi High Potential in the Lower Zambezi A way forward to sustainable development Delta Alliance Delta Alliance is an international knowledge network with the mission of improving the resilience of the world’s deltas, by bringing together people who live and work in the deltas. Delta Alliance has currently ten network Wings worldwide where activities are focused. Delta Alliance is exploring the possibility to connect the Zambezi Delta to this network and to establish a network Wing in Mozambique. WWF WWF is a worldwide organization with the mission to stop the degradation of the planet’s natural environment and build a future in which humans live in harmony with nature. WWF recently launched (June 2010) the World Estuary Alliance (WEA). WEA focuses on knowledge exchange and information sharing on the value of healthy estuaries and maximiza- tion of the potential and benefits of ‘natural systems’ in sustainable estuary development. In Mozambique WWF works amongst others in the Zambezi Basin and Delta on environmental flows and mangrove conservation. Frank Dekker (Delta Alliance) Wim van Driel (Delta Alliance) From 28 August to 2 September 2011, WWF and Delta Alliance have organized a joint mission to the Lower Zambezi Basin and Delta, in order to contribute to the sustainable development, knowing that large developments are just emerging. Bart Geenen (WWF) The delegation of this mission consisted of Companies (DHV and Royal Haskoning), NGOs (WWF), Knowledge Institutes (Wageningen University, Deltares, Alterra, and Eduardo Mondlane University) and Government Institutes (ARA Zambeze). -
Glimpopo Fact Sheet
Fact Sheet 1 The Limpopo River flows over a total distance of The Limpopo basin covers almost 14 percent of the total 1,750 kilometres. It starts at the confluence of the Marico area of its four riparian states – Botswana, South Africa, and Crocodile rivers in South Africa and flows northwest Zimbabwe and Mozambique. And of the basin’s total area, of Pretoria. It is joined by the Notwane river flowing from 44 percent is occupied by South Africa, 21 percent by Botswana, and then forms the border between Botswana Mozambique, almost 20 percent by Botswana and 16 per- and South Africa, and flows in a north easterly direction. cent by Zimbabwe. At the confluence of the Shashe river, which flows in from Zimbabwe and Botswana, the Limpopo turns almost due Drainage Network The Limpopo river has a rela- east and forms the border between Zimbabwe and South tively dense network of more than 20 tributary streams and Africa before entering Mozambique at Pafuri. For the next rivers, though most of these tributaries have either season- 561 km the river flows entirely within Mozambique and al or episodic flows. In historical times, the Limpopo river enters the Indian Ocean about 60 km downstream of the was a strong-flowing perennial river but is now regarded town of Xai-Xai. as a weak perennial river where flows frequently cease. During drought periods, no surface water is present over The Basin The Limpopo river basin is almost circular large stretches of the middle and lower reaches of the in shape with a mean altitude of 840 m above sea level.