Mpumalanga

The Lowveld is subtropical, due to its latitude and proximity to the warm Indian Ocean. The Highveld is comparatively much cooler, due to its altitude of 2300 m to 1700 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 severe frost, while the Lowveld is mostly frost-free. Winter rainfall is rare, except for some drizzle on the escarpment. The differences in climate are demonstrated below by the capital, Mbombela, which is in the Lowveld, an hour from Belfast 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

Farming
The climatic contrasts between the drier Highveld region, with its cold winters, and the hot, humid Lowveld allow for a variety of agricultural activities. 68% of Mpumalanga is used by agriculture. Crops include maize, wheat, sorghum, barley, sunflower seed, soybeans, macadamia’s, groundnuts, sugar cane, vegetables, coffee, tea, cotton, tobacco, citrus, subtropical and deciduous fruit.

Forestry is extensive around Sabie in the far north east of the province. Located near the forests, Ngodwana is the site of one of South Africa’s largest paper mills (Sappi).

Natural grazing covers approximately 14% of Mpumalanga. The main products are beef, mutton, wool, poultry and dairy.

Mining
Extensive mining is done and the minerals found include gold, platinum group metals, silica, chromite, vanadiferous magnetite, argentiferous zinc, antimony, cobalt, copper, iron, manganese, tin, coal, andalusite, chrysotile asbestos, kieselguhr, limestone, magnesite, talc and shale.

Gold was first discovered in Mpumalanga province in 1883 by Auguste Roberts in the mountains surrounding what is now Barberton. Gold is still mined in the Barberton area today.

Mpumalanga accounts for 83% of South Africa’s coal production. 90% of South Africa’s coal consumption is used for electricity generation and the synthetic fuel industry. Coal power stations are in proximity to the coal deposits. A coal liquefaction plant in Secunda (Secunda CTL) is one of the country’s two petroleum-from-coal extraction plants, which is operated by the synthetic fuel company Sasol.

The highveld region is the most polluted of the world due to the mine industry and plant power stations and the lowveld near the famous Kruger Park is under threat of new mines as well

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).

Mpumalanga is popular with tourists. Kruger National Park, established in 1898 for the protection of Lowveld wildlife, covering 20,000 square kilometres (7,700 sq mi), is a popular destination. The other major tourist attractions include the Sudwala Caves and the Blyde River Canyon.

Many activities including the big jump, mountain and quad biking, horse trails, river rafting and big game viewing are endemic to the region. This is “Big Five” territory. Towns in the Lowveld are Barberton, Mbombela, White River, Sabie, Graskop, Hazyview, Malelane, Pilgrim’s Rest, Lydenburg and Nkomazi.

In 2008, a Haute Cuisine route was formed, trickling from Mbombela down to Hazyview. The Lowveld Gourmet Route covers the four top fine dining restaurants the area has to offer. The restaurants include Summerfields Kitchen, Oliver’s Restaurant, Orange and Salt.

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. The Lydenburg Heads, from around 500 CE are Africa’s oldest iron age artworks south of the equator, and 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.

Under apartheid and colonialism, Mpumalanga was part of the Transvaal Province. The term “Eastern Transvaal” was used to refer to the eastern part of the province that became Mpumalanga in 1994.

The Mpumalanga Province’s legislation is an amalgam of national and regional legislation promulgated before the establishment of the province on 27 April 1994 and legislation which it has itself promulgated since it came into existence. Lists of and the original texts of this legislation are available through South African governmental websites. Amended and updated versions of the legislation is available through commercial vendors on subscription and at a price.