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Lydenburg

Lydenburg is a town in Thaba Chweu Local Municipality, on the Mpumalanga highveld, South Africa. It is situated on the Sterkspruit/Dorps River tributary of the Lepelle River at the summit of the Long Tom Pass. It has a long, rich history, ranging from AD 500 to the present. The name is derived from the Dutch Lijdenburg, or "Town of Suffering", and is named for the experiences of the white settlers. In Northern Sotho, Mashishing means "long green grass." Lydenburg has become the centre of the South African fly-fishing industry and is an agricultural, tourism and mining hub.

History

Ancient history

The area surrounding present day Lydenburg has a long history of human occupation. Rock paintings in surrounding areas point to early Khoe-San hunter-gather groups living on the land.

Lydenburg Heads

Dating back to AD 500, the earliest known forms of African Iron Age sculpture below the equator, known as the Lydenburg heads were found in the area. The seven earthenware sculptures of heads and other pottery from the site are intricately decorated and may have been used for ceremonial or initiation purposes. However, this is speculative as there is little we know today about the people who made these sculptures. Their existence nevertheless points to Lydenburg's remarkable heritage.

Pre-colonial History

From around the 16th century a group referred to as the Bakoni people occupied the area. There is evidence of Bapedi people, who referred to the area as Mashishing, that lived in the surrounding area from as early as the 1700s.

Colonial History

Founding of the town Lydenburg

Lydenburg was founded in 1849 by a group of Voortrekkers under the leadership of Andries Potgieter when they abandoned their previous settlement Ohrigstad (to the north) due to a malaria epidemic. The town became the capital of the Lydenburg Republic ('De Republiek Lydenburg in Zuid Afrika') in 1856 and later in 1857 joined the Republic of Utrecht but in 1860 both these republics joined the Zuid Afrikaanse Republiek (ZAR). The town became the capital of the Lydenburg District of the South African Republic (ZAR).

Lydenburg became important because it was on the wagon route to the port of Delagoa Bay (now Maputo Bay) which was not under British control. In 1871 construction of the road was started by Abraham Espag under the orders of President Thomas François Burgers. The first wagons arrived in Lydenburg from Delagoa Bay in 1874.

Gold Rush

On 6 February 1873, alluvial gold was discovered and within 3 months the Lydenburg goldfields were proclaimed. The First Boer War broke out between Britain and the Transvaal Republic in 1880. A British garrison under Lieutenant Walter Hillyar Colquhoun Long (uncle of the 1st Viscount Long) occupied Lydenburg to control the goldfields. It was from here that the ill-fated 94th Regiment under the command of Lieutenant-Colonel Philip Robert Anstruther marched to Pretoria. The remainder of the garrison at Lydenburg was besieged from 6 January 1881, following Long's refusal to surrender the garrison on 23 December 1880.

Land such as Boomplaats and Aapiesdoorndraai farms, near the town, was purchased by black South Africans in the early 1900s before the 1913 Land Act severely restricted black land ownership in South Africa. The communities here developed and irrigated the initially arid area into valuable and productive farms.

By 1910 the railway reached Lydenburg. In 1927 Lydenburg became a municipality.

Apartheid-Era History

Forced removals from farms surrounding Lydenburg began in the early 1940s and continued through the 1960s. Residents on the farms, especially through the ICU, ANC and local chiefs, resisted the removals in different ways depending on local circumstances and allegiances. Often violently, the apartheid state removed the families to farms further from the town or to Sekhukhuneland. In 2001, in one of South Africa's first completed land restitution claims, Boomplaats farm was bought from Willem Pretorius and returned by the state to the Dinkwanyane community.

Name change

In June 2006, it was announced that Arts and Culture minister, Pallo Jordan, had approved the renaming Lydenburg to Mashishing, meaning "wind blowing through the grass".

Mpumalanga

Mpumalanga (/əmˌpuːməˈlɑːŋɡə/) is a province of South Africa. The name means "East", or literally "The Place Where the Sun Rises" in the Swazi, Xhosa, Ndebele and Zulu languages. Mpumalanga lies in eastern South Africa, bordering Eswatini and Mozambique. It constitutes 6.5% of South Africa's land area. It shares borders with the South African provinces of Limpopo to the north, Gauteng to the west, the Free State to the southwest, and KwaZulu-Natal to the south. The capital is Mbombela. Mpumalanga was formed in 1994, when the area that was the Eastern Transvaal was merged with the former bantustans KaNgwane, KwaNdebele and parts of Lebowa and Gazankulu. Although the contemporary borders of the province were only formed at the end of apartheid, the region and its surroundings has a history that extends back thousands of years. Much of its history, and current significance is as a region of trade.

History

Precolonial Era

Archeological sites in the Mpumalanga region indicate settlement by humans and their ancestors dating back 1.7 million years. Rock paintings, engravings and other archeological evidence throughout the province indicate that Mpumalanga has a long history of human habitation by groups of hunter gathers. Excavations not far from the Mpumalanga border in the Origstad district, show evidence of Middle Stone Age habitation dating back to 40,000 years ago. The Lion Cavern, in Ngwenya on the Eswatini border, shows evidence of people mining iron ore in the Mpumalanga region and surrounding areas from at least 28 000 years ago. Evidence from mine shafts and trade goods shows that there was notable industry in tin, copper, gold, iron, ochre, and bronze. The Lydenburg Heads, from around 500 CE, are Africa's oldest Iron Age artworks south of the equator were found in Mpumalanga. Evidence from a site near Mbombela shows evidence of agricultural societies from between the 6th to 17th century. Bokoni stone-walled sites on the Mpumalanga highveld are indicative of a large precolonial agropastoral society between ~1500 and 1820 CE. These societies became centers of trade, with increasingly large and centralised populations, a pattern that increased as they connected to the Portuguese trading post in Maputo Bay. In this era, groups that would become the Swazi, Pedi, Ndebele, Mapulana and others established themselves in the area that is now Mpumalanga.

Colonial Era

In 1845, as part of the Great Trek, the first Dutch-speaking colonial settlers arrived in what they called the eastern Transvaal. The rest of the 19th century in the region was characterised by colonial encroachment and conflict over land and political control. In 1852, the Boers established the South African Republic. The well established Pedi, Swazi and Zulu kingdoms put up significant resistance against the settlers. The Pedi fought wars with the Boers in 1876 (see Sekhukhune Wars) and the Zulu fought with British settlers in 1879 (see Anglo-Zulu War). These interconnected conflicts played a role in shifting the balance of power in southern Africa to colonial control. After 1860, missionaries, especiailly German missionaries like Alexander Merensky set up mission stations in the region, spreading Christianity and European values. Just as the region had been a center for trade in the precolonial era, in the colonial era, the Eastern Transvaal region became an important thoroughfare for trade between Johannesburg and Delagoa Bay (now Maputo). Gold mining around areas like Pilgrims Rest and Barberton and farming were the main forms of economic activity. On farms in the Transvaal, under a system known as Inboekstelsel, Boers carried out raids to capture children and forced them into indentured labour. During the South African War, the region was the site of notable battles.

Apartheid

When the National Party came to power in 1948, their policy of apartheid intensified the segregation that had defined communities in the Transvaal. Under a policy of forced removals, Black South Africans were evicted from areas reserved for white people and moved into homelands, including KaNgwane, KwaNdebele, Lebowa and Gazankulu. As the apartheid regime implemented oppressive policies that defined almost every aspect of life, activists responded with resistance. In 1959, the small town of Bethal on what is now the Mpumalanga highveld was the center of the anti-apartheid consumer potato boycott in response to the working conditions Black South African labourers faced on farms in the area. The region was influenced by dynamics in exile and elsewhere in the country, for instance Black Consciousness, the Sharpeville Massacre and the 1976 Soweto Uprisings. In the 1980s, under intense repression, youth and labour organizations moblized against the government and townships and Bantustans erupted in political unrest and violence. In 1986, an avoidable disaster killed 177 mine workers in Kinross Mine in the region's highveld. The response to the disaster by the National Union of Mineworkers was a key point in the South African labour struggle. By the late 1980s, the intensity of resistance across South Africa (including areas like Mpumalanga, which hadn't previously been seen as key areas of resistance) combined with economic factors and international pressure was strong enough to end apartheid. On 27 April 1994, when South Africa held its first democratic elections, Mpumalanga province was formed. It was originally called the "Eastern Transvaal" province, but the name was later changed to Mpumalanga on the 24th of August 1995.

Post-apartheid

The liberation movement turned leading party, the African National Congress (ANC) came into power in Mpumalanga after white minority rule ended. A program of land redistribution, aimed at granting land back to the black communities who were forcibly moved during apartheid, had redistributed tens of thousands of hectares to these communities and their descendants. However, the process has been marked by corruption, controversy and has been seen as inadequate to address the extent of apartheid spatial planning. In 2001, 1,270 hectares of the Boomplaats farm near Mashishing was the first farm in South Africa to be expropriated. The post-apartheid era brought significant economic growth to Mpumalanga including notable progress in extending housing and basic services. However, poor governance, corruption and high levels of wealth and income inequality present persistent challenges to the province.

Geography

The Drakensberg escarpment divides Mpumalanga into a westerly half consisting mainly of high-altitude grassland called the Highveld and an eastern half situated in low-altitude subtropical Lowveld/Bushveld, mostly savanna habitat. The southern half of the Kruger National Park is in the latter region. The Drakensberg exceeds heights of 2000 m in most places, with this central region of Mpumalanga being very mountainous. These regions have alpine grasslands and small pockets of Afromontane forest. The Lowveld is relatively flat with interspersed rocky outcrops. The Lebombo Mountains form a low range in the far east, on the border with Mozambique.

Some of the oldest rocks on earth have been found in the Barberton area; these ancient greenstones and metamorphosed granites form the Crocodile River Mountains in the southeast of the province. The Lowveld is underlaid by African Cratonic Basement rocks of ages in excess of 2 billion years. The Highveld is mostly Karoo Sequence sedimentary rock of a younger, Carboniferous to Permian age.

Mpumalanga is the only South African province to border two provinces of Mozambique (Gaza Province to the northeast and Maputo Province to the east), as well as all four regions of Eswatini (Lubombo, Hhohho, Manzini, and Shiselweni Districts).

Climate

The Lowveld is subtropical, due to its latitude and proximity to the warm Indian Ocean. The Highveld is comparatively much cooler and drier, due to its elevation of 1700 m to 2300 m above sea level. The Drakensberg escarpment receives the most precipitation, with all other areas being moderately well-watered by mostly-summer thunderstorms. The Highveld often experiences considerable freezing, while the Lowveld is mostly frost-free. Winter rainfall is rare, except for some drizzle on the escarpment. The differences in climate are demonstrated by comparing the capital, Mbombela, which is in the Lowveld, with Belfast, which is an hour away on the Highveld:

• Mbombela averages: January maximum: 29 °C (min: 19 °C), July maximum: 23 °C (min: 6 °C), annual precipitation: 767 mm
• Belfast averages: January maximum: 23 °C (min: 12 °C), June maximum: 15 °C (min: 1 °C), annual precipitation: 878 mm

With climate change in the province, rainfall is becoming more variable, temperatures and evaporation rates are rising and extreme weather events are becoming more frequent. It is predicted that these changes will shift biomes so that most of the province will be savanna.

Ecology

Some of the earliest signs of life on Earth have been found in Mpumalanga. In the Makhonjwa mountain range's greenstone belt near Barberton, a fossil layer shows microbial activity that is 3.22 billion years old. This discovery indicates that life emerged on Earth 300 million years earlier than previously thought.

Mpumalanga has a high plant and animal diversity. Many species are endemic to the province.