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Historical Context
The broader Transvaal (meaning “across the Vaal” River) was one of South Africa’s four original provinces after the 1910 Union. It originated from the 19th-century South African Republic (ZAR), settled by Afrikaner Voortrekkers during the Great Trek in the 1830s. The region was rich in minerals (gold, platinum, coal, chromite) and became economically vital, especially the southern Witwatersrand area around Johannesburg.
In 1994, the large Transvaal province was divided into four new provinces as part of post-apartheid restructuring:
- Eastern Transvaal → Mpumalanga
- Northern Transvaal → Limpopo (mostly)
- Pretoria-Witwatersrand-Vereeniging (PWV) → Gauteng
- Parts of Western Transvaal → North West Province
This change incorporated former homelands (bantustans) like KaNgwane, KwaNdebele, and parts of Lebowa and Gazankulu.
Geography and Landscapes
Mpumalanga (formerly Eastern Transvaal) covers about 76,495 km² and features dramatic topographic diversity:
- Highveld (west): High-altitude grasslands (1,200–1,800 m), cooler and drier.
- Drakensberg Escarpment: Spectacular mountainous divide with peaks over 2,300 m, forests, waterfalls, and dramatic drops.
- Lowveld/Bushveld (east): Subtropical savanna plains sloping toward Mozambique, known for wildlife and hot, humid conditions.
Key features include the southern section of Kruger National Park (one of Africa’s premier wildlife destinations, part of the Great Limpopo Transfrontier Park), Blyde River Canyon (one of the largest canyons in the world), and rivers like the Crocodile, Olifants, and Sabie. The province borders Limpopo, Gauteng, Free State, KwaZulu-Natal, Eswatini (Swaziland), and Mozambique.
Climate
- Highveld/Drakensberg: Temperate, cooler winters (possible snow), mean ~16°C; rainfall 500–760 mm, mostly summer.
- Lowveld: Subtropical, hotter (mean ~23°C), humid summers, milder winters; higher rainfall in places (>1,000 mm). Precipitation generally increases eastward. Summers are warm-to-hot with thunderstorms; winters are dry and pleasant.
