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Pungwe Worm Snake
Pungwe River ( pt, Rio Púngoè, links=no or ''Rio Púnguè'') is a long river in Zimbabwe and Mozambique. It rises below Mount Nyangani in the Eastern Highlands of Zimbabwe and then flows southeasteastward through the Manica and Sofala provinces of Mozambique. The Pungwe enters the Urema Valley, the southernmost portion of the Great Rift Valley, where it forms the southern boundary of Gorongosa National Park. The Urema River joins it, and the river follows the rift valley southward. Large seasonal wetlands form around the Pungwe and Urema rivers in the rift valley section. It empties into the Mozambique Channel at Beira, forming a large estuary. It is one of the major rivers of Mozambique and often causes floods. Tributaries The principal left tributaries are, from upstream to downstream, the Nhazonia, Txatola, Vinduzi, and Nhandugue-Urema. The right tributaries are the Honde and the Muda. Pungwe basin Administratively, the Pungwe Basin covers parts of Sofala and Manica p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nyanga National Park
Nyanga National Park lies in the north of Zimbabwe's Eastern Highlands. One of the first national parks to be declared in the country,Nyanga National Park. Undated pamphlet, Zimbabwe Parks and Wildlife Authority it contains the highest land in Zimbabwe, with green hills and perennial rivers. Most of its terrain consists of rolling downland, sometimes lightly wooded, lying at altitudes between 1,800–2,593 metres (6,560–7,544 feet). Mount Nyangani, the highest point in Zimbabwe, lies in the centre of the park and Mutarazi Falls, Zimbabwe's highest waterfall, is in the south of the park. Nyanga National park incorporates the former Mutarazi Falls National Park on its southern boundary. History of the park The national park is one of the oldest in Zimbabwe, established as Rhodes Inyanga National Park, a bequest from Cecil Rhodes. The original park borders extended beyond Udu Dam, along the east bank of the Nyangombe River to the north of the current park boundary. This ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Rift Valley
The Great Rift Valley is a series of contiguous geographic trenches, approximately in total length, that runs from Lebanon in Asia to Mozambique in Southeast Africa. While the name continues in some usages, it is rarely used in geology as it is considered an imprecise merging of separate though related rift and fault systems. This valley extends northward for 5,950 km through the eastern part of Africa, through the Red Sea, and into Western Asia. Several deep, elongated lakes, called ribbon lakes, exist on the floor of this rift valley: Lakes Malawi, Rudolf and Tanganyika are examples of such lakes. The region has a unique ecosystem and contains a number of Africa's wildlife parks. The term Great Rift Valley is most often used to refer to the valley of the East African Rift, the divergent plate boundary which extends from the Afar Triple Junction southward through eastern Africa, and is in the process of splitting the African Plate into two new and separate plates. Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Mozambique
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Masterplan Beira 2035
Masterplan Beira 2035 is a program meant to overhaul the water management infrastructure for the city of Beira, Mozambique, with the intent of allowing for future urban development. The plan was created in partnership primarily between the city of Beira and the Dutch engineering and consultancy firm Witteveen+Bos. This perceived urban renewal is to help mitigate the effects of the increasing ferocity and frequency of environmental phenomena in the region, which has been heavily influenced by climate change. Background Beira is a coastal city that sits at a very low elevation, one that is only slightly above sea level. Due to this fact, as well as Mozambique's vulnerability to climate change, the city is becoming more susceptible to flooding and other water related issues. Furthermore, the city's coastal tide and sea overflow defenses, both natural and artificial, are failing. This has resulted in Coastal erosion, leading to severe flooding, which has numerous impacts on the communi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mutare
Mutare (formerly Umtali) is the most populous city in the province of Manicaland, and the third most populous city in Zimbabwe, having surpassed Gweru in the 2012 census, with an urban area, urban population of 224,802 and approximately 260,567 in the surrounding districts giving the wider metropolitan area a total population of over 500,000 people.http://www.zimstat.co.zw/wp-content/uploads/publications/Population/population/census-2012-national-report.pdf Mutare is also the capital of Manicaland province and the largest city in Eastern Zimbabwe. Located near the border with Mozambique, Mutare has long been a centre of trade and a key terminus en route to the port of Beira (in Beira, Mozambique). Mutare is hub for trade with railway links, pipeline transport and highways linking the coast with Harare and the interior. Other traditional industries include timber, papermaking, commerce, food processing, telecommunications, and transportation. In addition the city serves as a gat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nyanga District
Nyanga District is located in Manicaland Province of Zimbabwe. The administrative center is Nyanga village. The 2012 National Zimbabwe census reported its population to be 126,599 and being 52.2% female and 47.8% male. Geography Nyanga District is bounded on the south by Mutasa District, on the west by Makoni District, on the northwest by Mashonaland East Province, and on the east by Mozambique. The Nyanga Mountains occupy the southern portion of the district, extending into Mutasa District. Nyanga National Park covers the central part of the range, including Mount Nyangani, Zimbabwe's highest peak. The Gairezi River forms the eastern boundary of the District with Mozambique. The Nyangombe River forms the district's western and northwestern boundary. Both rivers flow generally northwards, and meet at the district's northernmost point to form the Luenha River, a tributary of the Zambezi. The Nyangui highlands lie in the center of the district. Nyangui State Forest was establis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mutasa District
Mutasa District is one of seven districts in Manicaland Province of Zimbabwe. Mutasa District is located 30 km northeast Mutare and stretches up to the Honde Valley, which is about 100 km northeast of Mutare along a tarred road that branches off the Nyanga road. Geography Mutasa District has an area of 2,548 km². Watsomba is the administrative headquarters. The district is bounded on the south and southwest by Mutare District, on the west by Makoni District, on the north by Nyanga District, and on the east and southeast by Mozambique. The Nyanga Mountains occupy the northern portion of the district, and a portion of Nyanga National Park is in the district. Mount Nyangani (2,592 m) is the highest peak in Zimbabwe. The northeastern corner of the district is in the upper watershed of the Gairezi River, which originates on Mt Nyangani and flows northward to meet the Zambezi. The Pungwe River also originates on Mount Nyangani. The Honde Valley lies south of the Nyan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sofala Province Mozambique 2009-03-12
Sofala, at present known as Nova Sofala, used to be the chief seaport of the Mwenemutapa Kingdom, whose capital was at Mount Fura. It is located on the Sofala Bank in Sofala Province of Mozambique. It was founded by Somali merchants. This name was given because the area is rich with resources.''The Horizon History of Africa'', vol. 1, p. 143 History One of the oldest harbours documented in Southern Africa, medieval Sofala was erected on the edge of a wide estuary formed by the Buzi River (called ''Rio de Sofala'' in older maps). The Buzi River connected Sofala to the internal market town of Manica, and from there to the gold fields of Great Zimbabwe. Sometime in the in 10th century,sofala emerged as a small trading post and was incorporated into the greater global Somali trade network. Merchants from the Sultanate of Mogadishu had long kept Sofala a secret from their Kilwan rivals, who up until then rarely sailed beyond Cape Delgado. In the 1180s, Sultan Suleiman Hassan of Kil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flooding In Mozambique Púnguè River 2010-03-08
A flood is an overflow of water ( or rarely other fluids) that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health. Human changes to the environment often increase the intensity and frequency of flooding, for example land use changes such as deforestation and removal of wetlands, changes in waterway course or flood controls such as with levees, and larger environmental issues such as climate change and sea level rise. In particular climate change's increased rainfall and extreme weather events increases the severity of other causes for flooding, resulting in more intense floods and increased flood risk. Flooding may occur as an overflow of water from water bodies, such as a river, lake, or ocean, in which the water overtops or breaks levees, resulting in some of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mozambique Channel
The Mozambique Channel (french: Canal du Mozambique, mg, Lakandranon'i Mozambika, pt, Canal de Moçambique) is an arm of the Indian Ocean located between the Southeast African countries of Madagascar and Mozambique. The channel is about long and across at its narrowest point, and reaches a depth of about off the coast of Mozambique. A warm current, the Mozambique Current, flows in a southward direction in the channel, leading into the Agulhas Current off the east coast of Southern Africa. Extent The International Hydrographic Organization (IHO) defines the limits of the Mozambique Channel as follows: ::''On the North.'' A line from the estuary of the River Rovuma () to Ras Habu, the northernmost point of Ile Grande Comore, the northernmost of the Comore (Comoro) Islands, to Cap d'Ambre (Cape Amber), the northern extremity of Madagascar (). ::''On the East.'' The west coast of Madagascar. ::''On the South.'' A line from Cap Sainte-Marie, the southern extremity of Mad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gorongosa National Park
Gorongosa National Park is at the southern end of the Great African Rift Valley in the heart of central Mozambique, Southeast Africa. The more than park comprises the valley floor and parts of surrounding plateaus. Rivers originating on nearby Mount Gorongosa () water the plain. Seasonal flooding and waterlogging of the valley, which is composed of a mosaic of soil types, creates a variety of distinct ecosystems. Grasslands are dotted with patches of acacia trees, savannah, dry forest on sands and seasonally rain-filled pans, and termite hill thickets. The plateaus contain miombo and montane forests and a spectacular rain forest at the base of a series of limestone gorges. This combination of unique features at one time supported some of the densest wildlife populations in all of Africa, including charismatic carnivores, herbivores, and over 500 bird species. But large mammal numbers were reduced by as much as 95% and ecosystems were stressed during the Mozambican Civil War (197 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
