Siphofaneni
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Siphofaneni
Siphofaneni is a town in the Lubombo Region of central Eswatini (Swaziland), 45 kilometres from Manzini and 20 kilometres from Big Bend, a major sugarcane-producing town on the main highway leading to Durban. It has a tropical climate, very hot during summer and cold in winter. Malaria is endemic in Lubombo. Siphofaneni has hot springs and is surrounded by several sugarcane farms. It is located on the banks of the largest river in Swaziland, the Usutu. Transports Siphofaneni has one of the main railway stations in the country, serving as a connection between the Goba railway (Matsapha-Siphofaneni-Mpaka) and the Richards Bay railway (Siphofaneni-Lavumisa). Goods trains of the Eswatini Railways Eswatini Railways (ESR), formerly known as Swaziland Railway or Swazi Rail, is the national railway corporation of Eswatini. Overview As in the rest of Southern Africa, the rail system of Eswatini is built to the narrow Cape gauge of . ESR pr ... pass through the town. References ...
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Goba Railway
Goba railway, also called Swaziland-Maputo railway and Matsapha-Maputo railway, is a railway that connects the city of Maputo, Mozambique, to the city from Matsapha, in Eswatini. It is 466.8 km long, in a 1067 mm gauge.Mozambique Logistics Infrastructure: Mozambique Railway Assessment
Atlassian Confluence. 10 de dezembro de 2018.
On the Mozambican stretch, between and , the managing company is
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Lubombo Region
Lubombo is a region of Eswatini, located in the east of the country. It has an area of 5,849.11 km² and a population of 212,531 (2017). Its administrative center is Siteki. It borders all three other regions: Hhohho to the north, Manzini to the west, and Shiselweni to the south. It is divided into 11 tinkhundla. Geography Geographically, the region is dominated almost entirely by the Lubombo Mountains. The Lubombo District is the easternmost of the four regions of Eswatini. Its capital is Siteki. Administrative divisions Lubombo is subdivided to 11 tinkhundla (or constituencies). These are local administration centres, and also parliamentary constituencies. Each inkhundla is headed by an ''indvuna yenkhundla'' or governor with the help of ''bucopho''. The tinkhundla are further divided into imiphakatsi (or chiefdoms). The present tinkhundla are: * Dvokodvweni ** Imiphakatsi: Enjabulweni, Etjedze, Malindza, Mampempeni, Mdumezulu, Mhlangatane, Sigcaweni * Hlane * ...
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Maputo River
The Maputo River (Portuguese ''Rio Maputo''), also called Great Usutu River, Lusutfu River, or Suthu River, is a river in South Africa, Eswatini, and Mozambique. The name ''Suthu'' refers to Basotho people who lived near the source of the river, but were attacked and displaced by Swazis. It is also said to mean 'dark brown', a description of the river's muddy water. Course The river rises near Amsterdam, Mpumalanga, South Africa, and flows easterly through Eswatini, where it enters the Lebombo Mountains. The 13 km gorge forms the boundary between Eswatini and South Africa. For approximately twenty kilometres, it forms the border between South Africa (province of KwaZulu-Natal) and Mozambique. There, in the Ndumo Game Reserve, it absorbs its largest tributary, the Pongola River. It then meanders through the Mozambican coastal plain and empties into southern Maputo Bay, some 85 kilometres downstream. In Eswatini, the river is called the Great Usutu or Lusutfu and flows throug ...
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Eswatini Railways
Eswatini Railways (ESR), formerly known as Swaziland Railway or Swazi Rail, is the national railway corporation of Eswatini. Overview As in the rest of Southern Africa, the rail system of Eswatini is built to the narrow Cape gauge of . ESR provides only service for transportation of goods, not passengers. ESR's rail system is used to connect the land-locked country to the sea. The east-west link, called the Goba line, leads from Matsapha (near Manzini) through Sidvokodvo, Phuzumoya and Mpaka to Goba in Mozambique. From Goba a Mozambique Ports and Railways line connects to the ports of Matola and Maputo. Swazi Rail also has two connections to South Africa: a northern link from Mpaka to Komatipoort in Mpumalanga on the Pretoria–Maputo railway, and a southern link from Phuzumoya to Golela in KwaZulu-Natal, from where the Transnet network connects to the ports of Richards Bay and Durban. History In 1902 the British administration of Eswatini agreed with the Portuguese ...
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Town
A town is a human settlement. Towns are generally larger than villages and smaller than cities, though the criteria to distinguish between them vary considerably in different parts of the world. Origin and use The word "town" shares an origin with the German word , the Dutch word , and the Old Norse . The original Proto-Germanic word, *''tūnan'', is thought to be an early borrowing from Proto-Celtic *''dūnom'' (cf. Old Irish , Welsh ). The original sense of the word in both Germanic and Celtic was that of a fortress or an enclosure. Cognates of ''town'' in many modern Germanic languages designate a fence or a hedge. In English and Dutch, the meaning of the word took on the sense of the space which these fences enclosed, and through which a track must run. In England, a town was a small community that could not afford or was not allowed to build walls or other larger fortifications, and built a palisade or stockade instead. In the Netherlands, this space was a garden, ...
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Eswatini
Eswatini ( ; ss, eSwatini ), officially the Kingdom of Eswatini and formerly named Swaziland ( ; officially renamed in 2018), is a landlocked country in Southern Africa. It is bordered by Mozambique to its northeast and South Africa to its north, west, south, and southeast. At no more than north to south and east to west, Eswatini is one of the smallest countries in Africa; despite this, its climate and topography are diverse, ranging from a cool and mountainous highveld to a hot and dry Veld, lowveld. The population is composed primarily of ethnic Swazi people, Swazis. The prevalent language is Swazi language, Swazi (''siSwati'' in native form). The Swazis established their kingdom in the mid-18th century under the leadership of Ngwane III. The country and the Swazi take their names from Mswati II, the 19th-century king under whose rule the country was expanded and unified; its boundaries were drawn up in 1881 in the midst of the Scramble for Africa. After the Second Boer W ...
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Manzini, Eswatini
Manzini (formerly known as ''Bremersdorp'') is a large city in Eswatini (Swaziland), which is also the capital of Eswatini's Manzini Region. The city is the country's largest urban center ahead of Mbabane, with a population of 110,000 (2008). It is known as "The Hub" of Eswatini and lies on the MR3 road. Eswatini's primary industrial site at Matsapha lies near the town's western border. History A commercial center from the time a trading post was opened in 1885, Bremersdorp was designated a township in 1898. Arthur Bremer sold his hotel for use as British Colonial authorities who had administered Swaziland since 1894 as their national administrative headquarters, and stipulated that the settlement would bear his name (''dorp'' is the Afrikaans word for "village"). The name reverted to its original Swazi name, Manzini, in 1960 in honor of Chief Manzini Mbokane who was one of the trusted confidant and senior indvuna of King Mbandzeni. Chief Manzini Mbokane was the father to Nteng ...
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Big Bend, Eswatini
Big Bend is a town in eastern Eswatini, lying on the Great Usutu River (Lusutfu). Its main industry is farming and it is based mostly on sugar plantations. Big Bend is also surrounded by nature/game reserves such as Mhlosinga Nature Reserve and Nisela Safaris. Schools Big Bend has several schools, such as The Edu-care Centre which is a preschool which caters to Swazi and expatriate children along with its sister schools, Ubombo Primary School and Sisekelo High School. They were established in the late 1970s and have pioneered the high level of teaching excellence in the kingdom that paved the way for other schools to follow. Climate Big Bend has a hot semi-arid climate A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi- ... ( Köppen: ''BSh'') with very hot and moderately rainy ...
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Sugarcane
Sugarcane or sugar cane is a species of (often hybrid) tall, perennial grass (in the genus '' Saccharum'', tribe Andropogoneae) that is used for sugar production. The plants are 2–6 m (6–20 ft) tall with stout, jointed, fibrous stalks that are rich in sucrose, which accumulates in the stalk internodes. Sugarcanes belong to the grass family, Poaceae, an economically important flowering plant family that includes maize, wheat, rice, and sorghum, and many forage crops. It is native to the warm temperate and tropical regions of India, Southeast Asia, and New Guinea. The plant is also grown for biofuel production, especially in Brazil, as the canes can be used directly to produce ethyl alcohol (ethanol). Grown in tropical and subtropical regions, sugarcane is the world's largest crop by production quantity, totaling 1.9 billion tonnes in 2020, with Brazil accounting for 40% of the world total. Sugarcane accounts for 79% of sugar produced globally (most of the re ...
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Tropical Climate
Tropical climate is the first of the five major climate groups in the Köppen climate classification identified with the letter A. Tropical climates are defined by a monthly average temperature of 18 °C (64.4 °F) or higher in the coolest month, and feature hot temperatures all year-round. Annual precipitation is often abundant in tropical climates, and shows a seasonal rhythm but may have seasonal dryness to varying degrees. There are normally only two seasons in tropical climates, a wet (rainy / monsoon) season and a dry season. The annual temperature range in tropical climates is normally very small. Sunlight is intense in these climates. There are three basic types of tropical climates within the tropical climate group: tropical rainforest climate (Af), tropical monsoon climate (Am) and tropical wet and dry climate or tropical savannah (Aw for dry winters, and As for dry summers), which are classified and distinguished by the precipitation and the precipitation lev ...
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Malaria
Malaria is a mosquito-borne infectious disease that affects humans and other animals. Malaria causes symptoms that typically include fever, tiredness, vomiting, and headaches. In severe cases, it can cause jaundice, seizures, coma, or death. Symptoms usually begin ten to fifteen days after being bitten by an infected mosquito. If not properly treated, people may have recurrences of the disease months later. In those who have recently survived an infection, reinfection usually causes milder symptoms. This partial resistance disappears over months to years if the person has no continuing exposure to malaria. Malaria is caused by single-celled microorganisms of the ''Plasmodium'' group. It is spread exclusively through bites of infected ''Anopheles'' mosquitoes. The mosquito bite introduces the parasites from the mosquito's saliva into a person's blood. The parasites travel to the liver where they mature and reproduce. Five species of ''Plasmodium'' can infect and be spread by h ...
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Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust ( pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ...
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